{"@context":{"@vocab":"https://cir.nii.ac.jp/schema/1.0/","rdfs":"http://www.w3.org/2000/01/rdf-schema#","dc":"http://purl.org/dc/elements/1.1/","dcterms":"http://purl.org/dc/terms/","foaf":"http://xmlns.com/foaf/0.1/","prism":"http://prismstandard.org/namespaces/basic/2.0/","cinii":"http://ci.nii.ac.jp/ns/1.0/","datacite":"https://schema.datacite.org/meta/kernel-4/","ndl":"http://ndl.go.jp/dcndl/terms/","jpcoar":"https://github.com/JPCOAR/schema/blob/master/2.0/"},"@id":"https://cir.nii.ac.jp/crid/1360020697621612160.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.5194/essd-15-5301-2023"}},{"identifier":{"@type":"URI","@value":"https://essd.copernicus.org/articles/15/5301/2023/essd-15-5301-2023.pdf"}},{"identifier":{"@type":"DOI","@value":"10.5194/essd-2023-409"}},{"identifier":{"@type":"DOI","@value":"10.5445/ir/1000169286"}},{"identifier":{"@type":"DOI","@value":"10.48350/195602"}},{"identifier":{"@type":"HANDLE","@value":"11370/0a35d98e-7c72-45be-bd11-2011be167343"}},{"identifier":{"@type":"HANDLE","@value":"21.11116/0000-000E-3750-A"}},{"identifier":{"@type":"HANDLE","@value":"21.11116/0000-000E-3745-7"}},{"identifier":{"@type":"HANDLE","@value":"21.11116/0000-000E-0341-5"}},{"identifier":{"@type":"HANDLE","@value":"21.11116/0000-000E-0343-3"}},{"identifier":{"@type":"HANDLE","@value":"21.11116/0000-000E-0344-2"}},{"identifier":{"@type":"HANDLE","@value":"20.500.11820/51ea39d1-51d3-4b9a-b276-841720504546"}},{"identifier":{"@type":"HANDLE","@value":"11250/3129018"}},{"identifier":{"@type":"HANDLE","@value":"10871/134742"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Global Carbon Budget 2023"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>Abstract. Accurate assessment of anthropogenic carbon dioxide (CO2) emissions and their redistribution among the atmosphere, ocean, and terrestrial biosphere in a changing climate is critical to better understand the global carbon cycle, support the development of climate policies, and project future climate change. Here we describe and synthesize data sets and methodology to quantify the five major components of the global carbon budget and their uncertainties. Fossil CO2 emissions (EFOS) are based on energy statistics and cement production data, while emissions from land-use change (ELUC), mainly deforestation, are based on land-use and land-use change data and bookkeeping models. Atmospheric CO2 concentration is measured directly, and its growth rate (GATM) is computed from the annual changes in concentration. The ocean CO2 sink (SOCEAN) is estimated with global ocean biogeochemistry models and observation-based fCO2 products. The terrestrial CO2 sink (SLAND) is estimated with dynamic global vegetation models. Additional lines of evidence on land and ocean sinks are provided by atmospheric inversions, atmospheric oxygen measurements, and Earth system models. The resulting carbon budget imbalance (BIM), the difference between the estimated total emissions and the estimated changes in the atmosphere, ocean, and terrestrial biosphere, is a measure of imperfect data and incomplete understanding of the contemporary carbon cycle. All uncertainties are reported as ±1σ. For the year 2022, EFOS increased by 0.9 % relative to 2021, with fossil emissions at 9.9±0.5 Gt C yr−1 (10.2±0.5 Gt C yr−1 when the cement carbonation sink is not included), and ELUC was 1.2±0.7 Gt C yr−1, for a total anthropogenic CO2 emission (including the cement carbonation sink) of 11.1±0.8 Gt C yr−1 (40.7±3.2 Gt CO2 yr−1). Also, for 2022, GATM was 4.6±0.2 Gt C yr−1 (2.18±0.1 ppm yr−1; ppm denotes parts per million), SOCEAN was 2.8±0.4 Gt C yr−1, and SLAND was 3.8±0.8 Gt C yr−1, with a BIM of −0.1 Gt C yr−1 (i.e. total estimated sources marginally too low or sinks marginally too high). The global atmospheric CO2 concentration averaged over 2022 reached 417.1±0.1 ppm. Preliminary data for 2023 suggest an increase in EFOS relative to 2022 of +1.1 % (0.0 % to 2.1 %) globally and atmospheric CO2 concentration reaching 419.3 ppm, 51 % above the pre-industrial level (around 278 ppm in 1750). Overall, the mean of and trend in the components of the global carbon budget are consistently estimated over the period 1959–2022, with a near-zero overall budget imbalance, although discrepancies of up to around 1 Gt C yr−1 persist for the representation of annual to semi-decadal variability in CO2 fluxes. Comparison of estimates from multiple approaches and observations shows the following: (1) a persistent large uncertainty in the estimate of land-use changes emissions, (2) a low agreement between the different methods on the magnitude of the land CO2 flux in the northern extra-tropics, and (3) a discrepancy between the different methods on the strength of the ocean sink over the last decade. This living-data update documents changes in methods and data sets applied to this most recent global carbon budget as well as evolving community understanding of the global carbon cycle. The data presented in this work are available at https://doi.org/10.18160/GCP-2023 (Friedlingstein et al., 2023).</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380020697621612191","@type":"Researcher","foaf:name":[{"@value":"Pierre Friedlingstein"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612056","@type":"Researcher","foaf:name":[{"@value":"Michael O'Sullivan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612205","@type":"Researcher","foaf:name":[{"@value":"Matthew W. Jones"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612179","@type":"Researcher","foaf:name":[{"@value":"Robbie M. Andrew"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612160","@type":"Researcher","foaf:name":[{"@value":"Dorothee C. E. Bakker"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612187","@type":"Researcher","foaf:name":[{"@value":"Judith Hauck"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612288","@type":"Researcher","foaf:name":[{"@value":"Peter Landschützer"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612212","@type":"Researcher","foaf:name":[{"@value":"Corinne Le Quéré"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612182","@type":"Researcher","foaf:name":[{"@value":"Ingrid T. Luijkx"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612041","@type":"Researcher","foaf:name":[{"@value":"Glen P. Peters"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612222","@type":"Researcher","foaf:name":[{"@value":"Wouter Peters"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612040","@type":"Researcher","foaf:name":[{"@value":"Julia Pongratz"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612053","@type":"Researcher","foaf:name":[{"@value":"Clemens Schwingshackl"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612223","@type":"Researcher","foaf:name":[{"@value":"Stephen Sitch"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612052","@type":"Researcher","foaf:name":[{"@value":"Josep G. Canadell"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612046","@type":"Researcher","foaf:name":[{"@value":"Philippe Ciais"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612172","@type":"Researcher","foaf:name":[{"@value":"Robert B. Jackson"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612218","@type":"Researcher","foaf:name":[{"@value":"Simone R. Alin"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612051","@type":"Researcher","foaf:name":[{"@value":"Peter Anthoni"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612037","@type":"Researcher","foaf:name":[{"@value":"Leticia Barbero"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612211","@type":"Researcher","foaf:name":[{"@value":"Nicholas R. Bates"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612047","@type":"Researcher","foaf:name":[{"@value":"Meike Becker"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612164","@type":"Researcher","foaf:name":[{"@value":"Nicolas Bellouin"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612058","@type":"Researcher","foaf:name":[{"@value":"Bertrand Decharme"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612044","@type":"Researcher","foaf:name":[{"@value":"Laurent Bopp"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612049","@type":"Researcher","foaf:name":[{"@value":"Ida Bagus Mandhara Brasika"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612035","@type":"Researcher","foaf:name":[{"@value":"Patricia Cadule"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612217","@type":"Researcher","foaf:name":[{"@value":"Matthew A. Chamberlain"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612054","@type":"Researcher","foaf:name":[{"@value":"Naveen Chandra"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612180","@type":"Researcher","foaf:name":[{"@value":"Thi-Tuyet-Trang Chau"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612225","@type":"Researcher","foaf:name":[{"@value":"Frédéric Chevallier"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612203","@type":"Researcher","foaf:name":[{"@value":"Louise P. Chini"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612162","@type":"Researcher","foaf:name":[{"@value":"Margot Cronin"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612193","@type":"Researcher","foaf:name":[{"@value":"Xinyu Dou"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612190","@type":"Researcher","foaf:name":[{"@value":"Kazutaka Enyo"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612294","@type":"Researcher","foaf:name":[{"@value":"Wiley Evans"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612177","@type":"Researcher","foaf:name":[{"@value":"Stefanie Falk"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612224","@type":"Researcher","foaf:name":[{"@value":"Richard A. Feely"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612064","@type":"Researcher","foaf:name":[{"@value":"Liang Feng"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612038","@type":"Researcher","foaf:name":[{"@value":"Daniel J. Ford"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612232","@type":"Researcher","foaf:name":[{"@value":"Thomas Gasser"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612220","@type":"Researcher","foaf:name":[{"@value":"Josefine Ghattas"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612200","@type":"Researcher","foaf:name":[{"@value":"Thanos Gkritzalis"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612062","@type":"Researcher","foaf:name":[{"@value":"Giacomo Grassi"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612185","@type":"Researcher","foaf:name":[{"@value":"Luke Gregor"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612184","@type":"Researcher","foaf:name":[{"@value":"Nicolas Gruber"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612173","@type":"Researcher","foaf:name":[{"@value":"Özgür Gürses"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612189","@type":"Researcher","foaf:name":[{"@value":"Ian Harris"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612059","@type":"Researcher","foaf:name":[{"@value":"Matthew Hefner"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612168","@type":"Researcher","foaf:name":[{"@value":"Jens Heinke"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612208","@type":"Researcher","foaf:name":[{"@value":"Richard A. Houghton"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612192","@type":"Researcher","foaf:name":[{"@value":"George C. Hurtt"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612221","@type":"Researcher","foaf:name":[{"@value":"Yosuke Iida"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612170","@type":"Researcher","foaf:name":[{"@value":"Tatiana Ilyina"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612219","@type":"Researcher","foaf:name":[{"@value":"Andrew R. Jacobson"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612199","@type":"Researcher","foaf:name":[{"@value":"Atul Jain"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612213","@type":"Researcher","foaf:name":[{"@value":"Tereza Jarníková"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612209","@type":"Researcher","foaf:name":[{"@value":"Annika Jersild"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612169","@type":"Researcher","foaf:name":[{"@value":"Fei Jiang"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612231","@type":"Researcher","foaf:name":[{"@value":"Zhe Jin"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612210","@type":"Researcher","foaf:name":[{"@value":"Fortunat Joos"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612204","@type":"Researcher","foaf:name":[{"@value":"Etsushi Kato"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612292","@type":"Researcher","foaf:name":[{"@value":"Ralph F. Keeling"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612227","@type":"Researcher","foaf:name":[{"@value":"Daniel Kennedy"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612033","@type":"Researcher","foaf:name":[{"@value":"Kees Klein Goldewijk"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612166","@type":"Researcher","foaf:name":[{"@value":"Jürgen Knauer"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612198","@type":"Researcher","foaf:name":[{"@value":"Jan Ivar Korsbakken"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612202","@type":"Researcher","foaf:name":[{"@value":"Arne Körtzinger"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612216","@type":"Researcher","foaf:name":[{"@value":"Xin Lan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612174","@type":"Researcher","foaf:name":[{"@value":"Nathalie Lefèvre"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612034","@type":"Researcher","foaf:name":[{"@value":"Hongmei Li"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612165","@type":"Researcher","foaf:name":[{"@value":"Junjie Liu"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612241","@type":"Researcher","foaf:name":[{"@value":"Zhiqiang Liu"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612215","@type":"Researcher","foaf:name":[{"@value":"Lei Ma"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612206","@type":"Researcher","foaf:name":[{"@value":"Greg Marland"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612239","@type":"Researcher","foaf:name":[{"@value":"Nicolas Mayot"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612171","@type":"Researcher","foaf:name":[{"@value":"Patrick C. McGuire"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612032","@type":"Researcher","foaf:name":[{"@value":"Galen A. McKinley"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612194","@type":"Researcher","foaf:name":[{"@value":"Gesa Meyer"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612167","@type":"Researcher","foaf:name":[{"@value":"Eric J. Morgan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612043","@type":"Researcher","foaf:name":[{"@value":"David R. Munro"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612289","@type":"Researcher","foaf:name":[{"@value":"Shin-Ichiro Nakaoka"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612207","@type":"Researcher","foaf:name":[{"@value":"Yosuke Niwa"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612181","@type":"Researcher","foaf:name":[{"@value":"Kevin M. O'Brien"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612196","@type":"Researcher","foaf:name":[{"@value":"Are Olsen"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612236","@type":"Researcher","foaf:name":[{"@value":"Abdirahman M. Omar"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612295","@type":"Researcher","foaf:name":[{"@value":"Tsuneo Ono"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612057","@type":"Researcher","foaf:name":[{"@value":"Melf Paulsen"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612042","@type":"Researcher","foaf:name":[{"@value":"Denis Pierrot"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612228","@type":"Researcher","foaf:name":[{"@value":"Katie Pocock"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612048","@type":"Researcher","foaf:name":[{"@value":"Benjamin Poulter"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612234","@type":"Researcher","foaf:name":[{"@value":"Carter M. Powis"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612240","@type":"Researcher","foaf:name":[{"@value":"Gregor Rehder"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612230","@type":"Researcher","foaf:name":[{"@value":"Laure Resplandy"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612293","@type":"Researcher","foaf:name":[{"@value":"Eddy Robertson"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612186","@type":"Researcher","foaf:name":[{"@value":"Christian Rödenbeck"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612290","@type":"Researcher","foaf:name":[{"@value":"Thais M. Rosan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612060","@type":"Researcher","foaf:name":[{"@value":"Jörg Schwinger"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612197","@type":"Researcher","foaf:name":[{"@value":"Roland Séférian"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612039","@type":"Researcher","foaf:name":[{"@value":"T. Luke Smallman"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612050","@type":"Researcher","foaf:name":[{"@value":"Stephen M. Smith"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612163","@type":"Researcher","foaf:name":[{"@value":"Reinel Sospedra-Alfonso"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612183","@type":"Researcher","foaf:name":[{"@value":"Qing Sun"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612214","@type":"Researcher","foaf:name":[{"@value":"Adrienne J. Sutton"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612188","@type":"Researcher","foaf:name":[{"@value":"Colm Sweeney"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612229","@type":"Researcher","foaf:name":[{"@value":"Shintaro Takao"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612238","@type":"Researcher","foaf:name":[{"@value":"Pieter P. Tans"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612237","@type":"Researcher","foaf:name":[{"@value":"Hanqin Tian"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612161","@type":"Researcher","foaf:name":[{"@value":"Bronte Tilbrook"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612175","@type":"Researcher","foaf:name":[{"@value":"Hiroyuki Tsujino"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612176","@type":"Researcher","foaf:name":[{"@value":"Francesco Tubiello"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612226","@type":"Researcher","foaf:name":[{"@value":"Guido R. van der Werf"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612061","@type":"Researcher","foaf:name":[{"@value":"Erik van Ooijen"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612201","@type":"Researcher","foaf:name":[{"@value":"Rik Wanninkhof"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612045","@type":"Researcher","foaf:name":[{"@value":"Michio Watanabe"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612195","@type":"Researcher","foaf:name":[{"@value":"Cathy Wimart-Rousseau"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612036","@type":"Researcher","foaf:name":[{"@value":"Dongxu Yang"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612063","@type":"Researcher","foaf:name":[{"@value":"Xiaojuan Yang"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612235","@type":"Researcher","foaf:name":[{"@value":"Wenping Yuan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612178","@type":"Researcher","foaf:name":[{"@value":"Xu Yue"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612055","@type":"Researcher","foaf:name":[{"@value":"Sönke Zaehle"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612291","@type":"Researcher","foaf:name":[{"@value":"Jiye Zeng"}]},{"@id":"https://cir.nii.ac.jp/crid/1380020697621612233","@type":"Researcher","foaf:name":[{"@value":"Bo Zheng"}]}],"contributor":[{"@id":"https://cir.nii.ac.jp/crid/1893118015718971525","@type":"Researcher","foaf:name":[{"@value":"Laboratoire des Sciences du Climat et de l'Environnement [Gif-sur-Yvette] (LSCE) ; Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)) ; Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)"}]},{"@id":"https://cir.nii.ac.jp/crid/1893118015718971572","@type":"Researcher","foaf:name":[{"@value":"Laboratoire de Météorologie Dynamique (UMR 8539) (LMD) ; Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X) ; Institut Polytechnique de Paris (IP Paris)-Institut Polytechnique de Paris (IP Paris)-École des Ponts ParisTech (ENPC)-Centre National de la Recherche Scientifique (CNRS)-Département des Géosciences - ENS Paris ; École normale supérieure - Paris (ENS-PSL) ; Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-École normale supérieure - Paris (ENS-PSL) ; Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)"}]},{"@id":"https://cir.nii.ac.jp/crid/1893118015718971691","@type":"Researcher","foaf:name":[{"@value":"Laboratoire de Météorologie Dynamique (UMR 8539) (LMD) ; Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X) ; Institut Polytechnique de Paris (IP Paris)-Institut Polytechnique de Paris (IP Paris)-École des Ponts ParisTech (ENPC)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Département des Géosciences - ENS Paris ; École normale supérieure - Paris (ENS-PSL) ; Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-École normale supérieure - Paris (ENS-PSL) ; Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)"}]},{"@id":"https://cir.nii.ac.jp/crid/1893118015718971527","@type":"Researcher","foaf:name":[{"@value":"Modélisation INVerse pour les mesures atmosphériques et SATellitaires (SATINV) ; Laboratoire des Sciences du Climat et de l'Environnement [Gif-sur-Yvette] (LSCE) ; Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)) ; Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)) ; Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)"}]},{"@id":"https://cir.nii.ac.jp/crid/1893118015718971581","@type":"Researcher","foaf:name":[{"@value":"Variabilité de l'Océan et de la Glace de mer (LOCEAN-VOG) ; Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques (LOCEAN) ; Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636)) ; École normale supérieure - Paris (ENS-PSL) ; Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X) ; Institut Polytechnique de Paris (IP Paris)-Institut Polytechnique de Paris (IP Paris)-Centre National d'Études Spatiales [Toulouse] (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité)-École normale supérieure - Paris (ENS-PSL) ; Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-École polytechnique (X) ; Institut Polytechnique de Paris (IP Paris)-Institut Polytechnique de Paris (IP Paris)-Centre National d'Études Spatiales [Toulouse] (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité)-Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636)) ; École normale supérieure - Paris (ENS-PSL) ; Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X) ; Institut Polytechnique de Paris (IP Paris)-Institut Polytechnique de Paris (IP Paris)-Centre National d'Études Spatiales [Toulouse] (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité)-École normale supérieure - Paris (ENS-PSL) ; Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-École polytechnique (X) ; Institut Polytechnique de Paris (IP Paris)-Institut Polytechnique de Paris (IP Paris)-Centre National d'Études Spatiales [Toulouse] (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité)"}]},{"@id":"https://cir.nii.ac.jp/crid/1893118015718971681","@type":"Researcher","foaf:name":[{"@value":"Centre national de recherches météorologiques (CNRM) ; Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP) ; Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3) ; Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3) ; Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS)"}]},{"@id":"https://cir.nii.ac.jp/crid/1893118015718971652","@type":"Researcher","foaf:name":[{"@value":"Variabilité de l'Océan et de la Glace de mer (VOG) ; Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques (LOCEAN) ; Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636)) ; École normale supérieure - Paris (ENS-PSL) ; Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X) ; Institut Polytechnique de Paris (IP Paris)-Institut Polytechnique de Paris (IP Paris)-Centre National d'Études Spatiales [Toulouse] (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité)-École normale supérieure - Paris (ENS-PSL) ; Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-École polytechnique (X) ; Institut Polytechnique de Paris (IP Paris)-Institut Polytechnique de Paris (IP Paris)-Centre National d'Études Spatiales [Toulouse] (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité)-Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636)) ; École normale supérieure - Paris (ENS-PSL) ; Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X) ; Institut Polytechnique de Paris (IP Paris)-Institut Polytechnique de Paris (IP Paris)-Centre National d'Études Spatiales [Toulouse] (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité)-École normale supérieure - Paris (ENS-PSL) ; Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-École polytechnique (X) ; Institut Polytechnique de Paris (IP Paris)-Institut Polytechnique de Paris (IP Paris)-Centre National d'Études Spatiales [Toulouse] (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité)"}]},{"@id":"https://cir.nii.ac.jp/crid/1893118015718971672","@type":"Researcher","foaf:name":[{"@value":"Dal Cin, Bruno"}]},{"@id":"https://cir.nii.ac.jp/crid/1893118015718971521","@type":"Researcher","foaf:name":[{"@value":"Aptel, Florence"}]},{"@id":"https://cir.nii.ac.jp/crid/1893118015718971570","@type":"Researcher","foaf:name":[{"@value":"Integr. Assessm. Global Environm. Change"}]},{"@id":"https://cir.nii.ac.jp/crid/1893118015718971654","@type":"Researcher","foaf:name":[{"@value":"Environmental Sciences"}]},{"@id":"https://cir.nii.ac.jp/crid/1893118015718971676","@type":"Researcher","foaf:name":[{"@value":"Laboratoire de Météorologie Dynamique (UMR 8539) (LMD) ; Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X)-École des Ponts ParisTech (ENPC)-Centre National de la Recherche Scientifique (CNRS)-Département des Géosciences - ENS Paris ; École normale supérieure - Paris (ENS-PSL) ; Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-École normale supérieure - Paris (ENS-PSL) ; Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)"}]},{"@id":"https://cir.nii.ac.jp/crid/1893118015718971393","@type":"Researcher","foaf:name":[{"@value":"Laboratoire des Sciences du Climat et de l'Environnement [Gif-sur-Yvette] (LSCE) ; Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)"}]},{"@id":"https://cir.nii.ac.jp/crid/1893118015718971556","@type":"Researcher","foaf:name":[{"@value":"Modélisation INVerse pour les mesures atmosphériques et SATellitaires (SATINV) ; Laboratoire des Sciences du Climat et de l'Environnement [Gif-sur-Yvette] (LSCE) ; Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)"}]},{"@id":"https://cir.nii.ac.jp/crid/1893118015718971530","@type":"Researcher","foaf:name":[{"@value":"Laboratoire de Météorologie Dynamique (UMR 8539) (LMD)"}]},{"@id":"https://cir.nii.ac.jp/crid/1893118015718971657","@type":"Researcher","foaf:name":[{"@value":"Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X)-École des Ponts ParisTech (ENPC)-Centre National de la Recherche Scientifique (CNRS)-Département des Géosciences - ENS Paris"}]},{"@id":"https://cir.nii.ac.jp/crid/1893118015718971567","@type":"Researcher","foaf:name":[{"@value":"École normale supérieure - Paris (ENS-PSL)"}]},{"@id":"https://cir.nii.ac.jp/crid/1893118015718971526","@type":"Researcher","foaf:name":[{"@value":"Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-École normale supérieure - Paris (ENS-PSL)"}]},{"@id":"https://cir.nii.ac.jp/crid/1893118015718971590","@type":"Researcher","foaf:name":[{"@value":"Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)"}]},{"@id":"https://cir.nii.ac.jp/crid/1893118015718971576","@type":"Researcher","foaf:name":[{"@value":"Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE)"}]},{"@id":"https://cir.nii.ac.jp/crid/1893118015718971582","@type":"Researcher","foaf:name":[{"@value":"Modélisation INVerse pour les mesures atmosphériques et SATellitaires (SATINV)"}]},{"@id":"https://cir.nii.ac.jp/crid/1893118015718971578","@type":"Researcher","foaf:name":[{"@value":"Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)"}]},{"@id":"https://cir.nii.ac.jp/crid/1893118015718971693","@type":"Researcher","foaf:name":[{"@value":"Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)"}]}],"publication":{"publicationIdentifier":[{"@type":"EISSN","@value":"18663516"}],"prism:publicationName":[{"@value":"Earth System Science Data"}],"dc:publisher":[{"@value":"Copernicus GmbH"}],"prism:publicationDate":"2023-12-05","prism:volume":"15","prism:number":"12","prism:startingPage":"5301","prism:endingPage":"5369"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","dc:rights":["https://creativecommons.org/licenses/by/4.0/"],"url":[{"@id":"https://essd.copernicus.org/articles/15/5301/2023/essd-15-5301-2023.pdf"}],"createdAt":"2023-11-30","modifiedAt":"2025-04-14","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=%5BSDU.OCEAN%5DSciences%20of%20the%20Universe%20%5Bphysics%5D/Ocean,%20Atmosphere","dc:title":"[SDU.OCEAN]Sciences of the Universe [physics]/Ocean, Atmosphere"},{"@id":"https://cir.nii.ac.jp/all?q=%5BSDU.OCEAN%5DSciences%20of%20the%20Universe%20%5Bphysics%5D/Ocean","dc:title":"[SDU.OCEAN]Sciences of the Universe [physics]/Ocean"},{"@id":"https://cir.nii.ac.jp/all?q=Atmosphere","dc:title":"Atmosphere"},{"@id":"https://cir.nii.ac.jp/all?q=%5BSDU.OCEAN%5D%20Sciences%20of%20the%20Universe%20%5Bphysics%5D/Ocean,%20Atmosphere","dc:title":"[SDU.OCEAN] Sciences of the Universe [physics]/Ocean, Atmosphere"},{"@id":"https://cir.nii.ac.jp/all?q=530%20Physics","dc:title":"530 Physics"},{"@id":"https://cir.nii.ac.jp/all?q=551","dc:title":"551"},{"@id":"https://cir.nii.ac.jp/all?q=333","dc:title":"333"},{"@id":"https://cir.nii.ac.jp/all?q=%5BSDU.ENVI%5D%20Sciences%20of%20the%20Universe%20%5Bphysics%5D/Continental%20interfaces,%20environment","dc:title":"[SDU.ENVI] Sciences of the Universe [physics]/Continental interfaces, environment"},{"@id":"https://cir.nii.ac.jp/all?q=%5BSDU.STU.CL%5D%20Sciences%20of%20the%20Universe%20%5Bphysics%5D/Earth%20Sciences/Climatology","dc:title":"[SDU.STU.CL] Sciences of the Universe [physics]/Earth Sciences/Climatology"},{"@id":"https://cir.nii.ac.jp/all?q=%5BSDU.STU.CL%5DSciences%20of%20the%20Universe%20%5Bphysics%5D/Earth%20Sciences/Climatology","dc:title":"[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology"},{"@id":"https://cir.nii.ac.jp/all?q=Life%20Science","dc:title":"Life Science"},{"@id":"https://cir.nii.ac.jp/all?q=%5BSDU.ENVI%5DSciences%20of%20the%20Universe%20%5Bphysics%5D/Continental%20interfaces","dc:title":"[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces"},{"@id":"https://cir.nii.ac.jp/all?q=%5BSDU.ENVI%5DSciences%20of%20the%20Universe%20%5Bphysics%5D/Continental%20interfaces,%20environment","dc:title":"[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces, environment"},{"@id":"https://cir.nii.ac.jp/all?q=environment","dc:title":"environment"}],"project":[{"@id":"https://cir.nii.ac.jp/crid/1040018351904855296","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"23K28206"},{"@type":"JGN","@value":"JP23K28206"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-23K28206/"}],"notation":[{"@language":"ja","@value":"北太平洋中高緯度域の新生産に貢献するケイ藻類と窒素固定ラン藻類の動態変化の解明"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050580914958226688","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Limited impact of hydrogen co-firing on prolonging fossil-based power generation under low emissions scenarios"}]},{"@id":"https://cir.nii.ac.jp/crid/1360001114155912960","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Impact of changes in diffuse radiation on the global land carbon sink"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011142931999872","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Global burned area and biomass burning emissions from small fires"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011142933191040","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Estimates of European uptake of CO\n                    <sub>2</sub>\n                    inferred from GOSAT X\n                    <sub>\n                      CO\n                      <sub>2</sub>\n                    </sub>\n                    retrievals: sensitivity to measurement bias inside and outside Europe"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011142933838080","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Evaluation of spatially explicit emission scenario of land-use change and biomass burning using a process-based biogeochemical model"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011142936313600","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Global and regional drivers of accelerating CO\n            <sub>2</sub>\n            emissions"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011142937015680","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"World ocean heat content and thermosteric sea level change (0–2000 m), 1955–2010"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011142937065984","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Unexpectedly large impact of forest management and grazing on global vegetation biomass"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011142939772288","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A human-driven decline in global burned area"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011143593556992","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Decadal Climate Prediction Project (DCPP) contribution to CMIP6"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011144347754240","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"CO\n                    <sub>2</sub>\n                    flux history 1982–2001 inferred from atmospheric data using a global inversion of atmospheric transport"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011144357344384","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Five decades of northern land carbon uptake revealed by the interhemispheric CO2 gradient"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011146102227584","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Atmospheric Lifetime of Fossil Fuel Carbon Dioxide"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011146239441664","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The reinvigoration of the Southern Ocean carbon sink"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011146328181376","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Fossil CO2 emissions in the post-COVID-19 era"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011146550227968","@type":"Article","resourceType":"preprint","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Predictable Variations of the Carbon Sinks and Atmospheric CO<sub>2</sub> Growth in a Multi‐Model Framework"}]},{"@id":"https://cir.nii.ac.jp/crid/1360013170976418048","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The sponge effect and carbon emission mitigation potentials of the global cement cycle"}]},{"@id":"https://cir.nii.ac.jp/crid/1360013171638363776","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Reaching peak emissions"}]},{"@id":"https://cir.nii.ac.jp/crid/1360013171943009152","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"External Forcing Explains Recent Decadal Variability of the Ocean Carbon Sink"}]},{"@id":"https://cir.nii.ac.jp/crid/1360016864418008192","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Surface ocean CO2 concentration and air-sea flux estimate by machine learning with modelled variable trends"}]},{"@id":"https://cir.nii.ac.jp/crid/1360016867498280960","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Copernicus Global 1/12° Oceanic and Sea Ice GLORYS12 Reanalysis"}]},{"@id":"https://cir.nii.ac.jp/crid/1360016868141558144","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Quantifying Errors in Observationally Based Estimates of Ocean Carbon Sink Variability"}]},{"@id":"https://cir.nii.ac.jp/crid/1360016868508267008","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Collection 6 MODIS burned area mapping algorithm and product"}]},{"@id":"https://cir.nii.ac.jp/crid/1360016870037555072","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"SeaFlux: harmonization of air–sea CO\n                    <sub>2</sub>\n                    fluxes from surface\n                    <i>p</i>\n                    CO\n                    <sub>2</sub>\n                    data products using a standardized approach"}]},{"@id":"https://cir.nii.ac.jp/crid/1360016870449517312","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A seamless ensemble-based reconstruction of surface ocean\n                    <i>p</i>\n                    CO\n                    <sub>2</sub>\n                    and air–sea CO\n                    <sub>2</sub>\n                    fluxes over the global coastal and open oceans"}]},{"@id":"https://cir.nii.ac.jp/crid/1360016870449524608","@type":"Article","resourceType":"preprint","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Global Carbon Budget 2021"}]},{"@id":"https://cir.nii.ac.jp/crid/1360017285972602496","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Changing State of the Climate System"}]},{"@id":"https://cir.nii.ac.jp/crid/1360017286996719872","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Global CO\n                    <sub>2</sub>\n                    uptake by cement from 1930 to 2019"}]},{"@id":"https://cir.nii.ac.jp/crid/1360017287038678656","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Global Carbon and Other Biogeochemical Cycles and Feedbacks"}]},{"@id":"https://cir.nii.ac.jp/crid/1360017287044426496","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Estimated regional CO\n                    <sub>2</sub>\n                    flux and uncertainty based on an ensemble of atmospheric CO\n                    <sub>2</sub>\n                    inversions"}]},{"@id":"https://cir.nii.ac.jp/crid/1360021396128055552","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Are Terrestrial Biosphere Models Fit for Simulating the Global Land Carbon Sink?"}]},{"@id":"https://cir.nii.ac.jp/crid/1360025429436763136","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Mapping seamless monthly XCO2 in East Asia: Utilizing OCO-2 data and machine learning"}]},{"@id":"https://cir.nii.ac.jp/crid/1360025431130522368","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Experimental studies on CO2 sequestration via enhanced rock weathering in seawater: Insights for climate change mitigation strategies in coastal and open ocean environments"}]},{"@id":"https://cir.nii.ac.jp/crid/1360025439243010688","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Assessing the size and uncertainty of remaining carbon budgets"}]},{"@id":"https://cir.nii.ac.jp/crid/1360026060099171968","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The JapanFlux2024 dataset for eddy covariance observations covering Japan and East Asia from 1990 to 2023"}]},{"@id":"https://cir.nii.ac.jp/crid/1360282588984836992","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Weak Northern and Strong Tropical Land Carbon Uptake from Vertical Profiles of Atmospheric CO\n                    <sub>2</sub>"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283696095412096","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A uniform, quality controlled Surface Ocean CO\n                    <sub>2</sub>\n                    Atlas (SOCAT)"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292617909636864","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Uncertainty in the response of terrestrial carbon sink to environmental drivers undermines carbon-climate feedback predictions"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292617910412544","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Inferring CO\n                    <sub>2</sub>\n                    sources and sinks from satellite observations: Method and application to TOVS data"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292617913312256","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Global fire emissions estimates during 1997–2016"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292617915757184","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Historical (1750–2014) anthropogenic emissions of reactive gases and aerosols from the Community Emissions Data System (CEDS)"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292617916221056","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Recent increase in oceanic carbon uptake driven by weaker upper-ocean overturning"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292619380692992","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Decadal variations and trends of the global ocean carbon sink"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292619747397888","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"How have past fire disturbances contributed to the current carbon balance of  boreal ecosystems?"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292619853003648","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Asynchronous carbon sink saturation in African and Amazonian tropical forests"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292620346524544","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Contributions to accelerating atmospheric CO\n                    <sub>2</sub>\n                    growth from economic activity, carbon intensity, and efficiency of natural sinks"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292620500091776","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Mechanisms governing interannual variability in upper-ocean inorganic carbon system and air–sea CO2 fluxes: Physical climate and atmospheric dust"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292620963486976","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Agreement of CMIP5 Simulated and Observed Ocean Anthropogenic CO<sub>2</sub> Uptake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292621553758720","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"On the long-term stability of reference gases for atmospheric O<sub>2</sub>/N<sub>2</sub>and CO<sub>2</sub>measurements"}]},{"@id":"https://cir.nii.ac.jp/crid/1360294645353136896","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Satellite-based time-series of sea-surface temperature since 1981 for climate applications"}]},{"@id":"https://cir.nii.ac.jp/crid/1360294646864118656","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Reassessing Southern Ocean Air‐Sea CO<sub>2</sub> Flux Estimates With the Addition of Biogeochemical Float Observations"}]},{"@id":"https://cir.nii.ac.jp/crid/1360294647055566592","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Increasing forest fire emissions despite the decline in global burned area"}]},{"@id":"https://cir.nii.ac.jp/crid/1360294647258274688","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Reconciling global-model estimates and country reporting of anthropogenic forest CO2 sinks"}]},{"@id":"https://cir.nii.ac.jp/crid/1360294647881306752","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Gridded fossil CO2 emissions and related O2 combustion consistent with national inventories 1959–2018"}]},{"@id":"https://cir.nii.ac.jp/crid/1360294647913222912","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Importance of El Niño reproducibility for reconstructing historical CO\n                    <sub>2</sub>\n                    flux variations in the equatorial Pacific"}]},{"@id":"https://cir.nii.ac.jp/crid/1360294648022144768","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Terminology as a key uncertainty in net land use and land cover change carbon flux estimates"}]},{"@id":"https://cir.nii.ac.jp/crid/1360298345007368704","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Global Carbon Budget 2022"}]},{"@id":"https://cir.nii.ac.jp/crid/1360298345081514880","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"OceanSODA-ETHZ: a global gridded data set of the surface ocean carbonate system for seasonal to decadal studies of ocean acidification"}]},{"@id":"https://cir.nii.ac.jp/crid/1360298761974250624","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Revision of the World Meteorological Organization Global Atmosphere Watch (WMO/GAW) CO\n                    <sub>2</sub>\n                    calibration scale"}]},{"@id":"https://cir.nii.ac.jp/crid/1360298761979306368","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Global and regional drivers of land-use emissions in 1961–2017"}]},{"@id":"https://cir.nii.ac.jp/crid/1360298762777316736","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The impact of alternative trait‐scaling hypotheses for the maximum photosynthetic carboxylation rate (<i>V</i><sub>cmax</sub>) on global gross primary production"}]},{"@id":"https://cir.nii.ac.jp/crid/1360298765126819200","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The PRIMAP-hist national historical emissions time series"}]},{"@id":"https://cir.nii.ac.jp/crid/1360298765190829184","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Decadal trends in the ocean carbon sink"}]},{"@id":"https://cir.nii.ac.jp/crid/1360298765202272128","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Have Synergies Between Nitrogen Deposition and Atmospheric CO<sub>2</sub> Driven the Recent Enhancement of the Terrestrial Carbon Sink?"}]},{"@id":"https://cir.nii.ac.jp/crid/1360302866835018368","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Magnitude, Trends, and Variability of the Global Ocean Carbon Sink From 1985 to 2018"}]},{"@id":"https://cir.nii.ac.jp/crid/1360302868519834112","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Indicators of Global Climate Change 2022: annual update of large-scale indicators of the state of the climate system and human influence"}]},{"@id":"https://cir.nii.ac.jp/crid/1360302868778250240","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Development of a REgion‐Specific Ecosystem Feedback Fire (RESFire) Model in the Community Earth System Model"}]},{"@id":"https://cir.nii.ac.jp/crid/1360302868778251776","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Evaluation of an Online Grid‐Coarsening Algorithm in a Global Eddy‐Admitting Ocean Biogeochemical Model"}]},{"@id":"https://cir.nii.ac.jp/crid/1360302868778255104","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Amplification of the Ocean Carbon Sink During El Niños: Role of Poleward Ekman Transport and Influence on Atmospheric CO<sub>2</sub>"}]},{"@id":"https://cir.nii.ac.jp/crid/1360302868778256384","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Air‐Sea Fluxes of CO<sub>2</sub> in the Indian Ocean Between 1985 and 2018: A Synthesis Based on Observation‐Based Surface CO<sub>2</sub>, Hindcast and Atmospheric Inversion Models"}]},{"@id":"https://cir.nii.ac.jp/crid/1360302868778278528","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Process-oriented analysis of dominant sources of uncertainty in the land carbon sink"}]},{"@id":"https://cir.nii.ac.jp/crid/1360302868778286976","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Regional Wind Variability Modulates the Southern Ocean Carbon Sink"}]},{"@id":"https://cir.nii.ac.jp/crid/1360302868778375808","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The transition from deforestation to reforestation in Europe."}]},{"@id":"https://cir.nii.ac.jp/crid/1360302868778650880","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Where does the carbon go? A model–data intercomparison of vegetation carbon allocation and turnover processes at two temperate forest free‐air CO<sub>2</sub> enrichment sites"}]},{"@id":"https://cir.nii.ac.jp/crid/1360302868779121408","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Regional CO\n                    <sub>2</sub>\n                    fluxes from 2010 to 2015 inferred from GOSAT XCO\n                    <sub>2</sub>\n                    retrievals using a new version of the Global Carbon Assimilation System"}]},{"@id":"https://cir.nii.ac.jp/crid/1360302868779131136","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Comparing the influence of net and gross anthropogenic land-use and land-cover changes on the carbon cycle in the MPI-ESM"}]},{"@id":"https://cir.nii.ac.jp/crid/1360302868779132032","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Historical CO\n                    <sub>2</sub>\n                    emissions from land use and land cover change and their uncertainty"}]},{"@id":"https://cir.nii.ac.jp/crid/1360302868779133440","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Global evaluation of terrestrial biogeochemistry in the Energy Exascale Earth System Model (E3SM) and the role of the phosphorus cycle in the historical terrestrial carbon balance"}]},{"@id":"https://cir.nii.ac.jp/crid/1360302868779134720","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Parameter uncertainty dominates C-cycle forecast  errors over most of Brazil for the 21st century"}]},{"@id":"https://cir.nii.ac.jp/crid/1360302868779135744","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Comparison of uncertainties in land-use change  fluxes from bookkeeping model parameterisation"}]},{"@id":"https://cir.nii.ac.jp/crid/1360302868779136768","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Carbon emissions and removals from forests: new estimates, 1990–2020"}]},{"@id":"https://cir.nii.ac.jp/crid/1360302868779138048","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Annual emissions of carbon from land use, land-use change, and forestry from 1850 to 2020"}]},{"@id":"https://cir.nii.ac.jp/crid/1360302868779138816","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Representation of fire, land-use change and vegetation dynamics in the Joint UK Land Environment Simulator vn4.9 (JULES)"}]},{"@id":"https://cir.nii.ac.jp/crid/1360302868779140352","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"CLASSIC v1.0: the open-source community successor to the Canadian Land Surface Scheme (CLASS) and the Canadian Terrestrial Ecosystem Model (CTEM) – Part 1: Model framework and site-level performance"}]},{"@id":"https://cir.nii.ac.jp/crid/1360302868779142016","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Ocean biogeochemistry in the coupled ocean–sea ice–biogeochemistry model FESOM2.1–REcoM3"}]},{"@id":"https://cir.nii.ac.jp/crid/1360302869429164160","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"History of El Niño impacts on the global carbon cycle 1957–2017: a quantification from atmospheric CO\n            <sub>2</sub>\n            data"}]},{"@id":"https://cir.nii.ac.jp/crid/1360302870127328128","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Author Correction: Temperature extremes of 2022 reduced carbon uptake by forests in Europe"}]},{"@id":"https://cir.nii.ac.jp/crid/1360302870129339136","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The land-to-ocean loops of the global carbon cycle"}]},{"@id":"https://cir.nii.ac.jp/crid/1360306509099852800","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Global burned area increasingly explained by climate change"}]},{"@id":"https://cir.nii.ac.jp/crid/1360306904402662016","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Extension of Japan’s Prefectural Emission Accounting and Enrichment of Socioeconomic Data from 1990 to 2020"}]},{"@id":"https://cir.nii.ac.jp/crid/1360306905168968320","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Handling modular containers in a physical internet environment"}]},{"@id":"https://cir.nii.ac.jp/crid/1360306905642076416","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Utilizing Magnesium Carbonate Induced by CO2 to Modify the Performance of Plastic Clay"}]},{"@id":"https://cir.nii.ac.jp/crid/1360564064110327680","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Global carbon budget 2013"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565165351553024","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Uptake mechanism of anthropogenic CO2 in the Kuroshio Extension region in an ocean general circulation model"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567185910137856","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The oceanic sink for anthropogenic CO\n            <sub>2</sub>\n            from 1994 to 2007"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574092883938688","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Global Carbon Budget 2015"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574092884886528","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Global Carbon Budget 2019"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574092886284416","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Reduced carbon emission estimates from fossil fuel combustion and cement production in China"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574092886620800","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Reviews and syntheses: An empirical spatiotemporal description of the global surface–atmosphere carbon fluxes: opportunities and data limitations"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574092890849024","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Estimating surface CO\n                    <sub>2</sub>\n                    fluxes from space-borne CO\n                    <sub>2</sub>\n                    dry air mole fraction observations using an ensemble Kalman Filter"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574092891537792","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Tropical forests are a net carbon source based on aboveground measurements of gain and loss"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574092892928640","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Compensatory water effects link yearly global land CO2 sink changes to temperature"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574092893304832","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Global Carbon Budget 2016"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574093669569792","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A multi-decade record of high-quality\n                    <i>f</i>\n                    CO\n                    <sub>2</sub>\n                    data in version 3 of the Surface Ocean CO\n                    <sub>2</sub>\n                    Atlas (SOCAT)"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574093781420032","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Evaluation of the terrestrial carbon cycle, future plant geography and climate‐carbon cycle feedbacks using five Dynamic Global Vegetation Models (DGVMs)"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574094230317056","@type":"Article","resourceType":"preprint","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Global carbon budget 2014"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574094459419776","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Atmospheric carbon dioxide variations at Mauna Loa Observatory, Hawaii"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574095371801472","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Riverine‐driven interhemispheric transport of carbon"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574095522505344","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Impact of climate change and variability on the global oceanic sink of CO<sub>2</sub>"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574095622759168","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Global Land Carbon Cycle Simulated With ISBA‐CTRIP: Improvements Over the Last Decade"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574095983060480","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Uncertainties around reductions in China’s coal use and CO2 emissions"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574096335091584","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"An ensemble data assimilation system to estimate CO\n                    <sub>2</sub>\n                    surface fluxes from atmospheric trace gas observations"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574096357694720","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Revised estimates of ocean-atmosphere CO2 flux are consistent with ocean carbon inventory"}]},{"@id":"https://cir.nii.ac.jp/crid/1360576121771133312","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Critical adjustment of land mitigation pathways for assessing countries’ climate progress"}]},{"@id":"https://cir.nii.ac.jp/crid/1360580235821939840","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Integrating the evidence for a terrestrial carbon sink caused by increasing atmospheric CO\n                    <sub>2</sub>"}]},{"@id":"https://cir.nii.ac.jp/crid/1360580235937468800","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Vast CO2 release from Australian fires in 2019–2020 constrained by satellite"}]},{"@id":"https://cir.nii.ac.jp/crid/1360580236951795072","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Soil moisture–atmosphere feedback dominates land carbon uptake variability"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584343730486144","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Role of jellyfish in the plankton ecosystem revealed using a global ocean biogeochemical model"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584343744230656","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Trends and variability in the ocean carbon sink"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584343744440832","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Quantifying global carbon dioxide removal deployment"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584343744921728","@type":"Article","resourceType":"preprint","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Decadal Trends in the Oceanic Storage of Anthropogenic Carbon from 1994 to 2014"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584345440083328","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Increased influence of nitrogen limitation on CO<sub>2</sub> emissions from future land use and land use change"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584345440165888","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The First Global Carbon Dioxide Flux Map Derived from TanSat Measurements"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584345440628736","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Emerging threats linking tropical deforestation and the COVID-19 pandemic"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584345440769536","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Variability in the Global Ocean Carbon Sink From 1959 to 2020 by Correcting Models With Observations"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584345440787968","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Drivers of declining CO2 emissions in 18 developed economies"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584345440853760","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Distinguishing disturbance from perturbations in fire-prone ecosystems"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584345440946816","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A multi-data assessment of land use and land cover emissions from Brazil during 2000–2019"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584345440948736","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Aerosol–light interactions reduce the carbon budget imbalance"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584345440950144","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Global fossil carbon emissions rebound near pre-COVID-19 levels"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584345440952064","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Land-use change emissions based on high-resolution activity data substantially lower than previously estimated"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584345441275520","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"FluxEngine: A Flexible Processing System for Calculating Atmosphere–Ocean Carbon Dioxide Gas Fluxes and Climatologies"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584345441662208","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Land-use and land-cover change carbon emissions between 1901 and 2012 constrained by biomass observations"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584345441665280","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Observation-constrained estimates of the global ocean carbon sink from Earth system models"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584345441666304","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Timely estimates of India's annual and monthly fossil CO\n                    <sub>2</sub>\n                    emissions"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584345441667200","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Harmonising the land-use flux estimates of global models and national inventories for 2000–2020"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584345441670656","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Accounting for carbon and nitrogen interactions in the global terrestrial ecosystem model ORCHIDEE (trunk version, rev 4999): multi-scale evaluation of gross primary production"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584345441672320","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Definitions and methods to estimate regional land carbon fluxes for the second phase of the REgional Carbon Cycle Assessment and Processes Project (RECCAP-2)"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584345441675392","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Global evaluation of the Ecosystem Demography model (ED v3.0)"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584345441678208","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Yale Interactive terrestrial Biosphere model version 1.0: description, evaluation and implementation into NASA GISS ModelE2"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584345441678976","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The FluxEngine air–sea gas flux toolbox: simplified interface and extensions for in situ analyses and multiple sparingly soluble gases"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584346083599744","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Data-based estimates of interannual sea–air CO\n                    <sub>2</sub>\n                    flux variations 1957–2020 and their relation to environmental drivers"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584346083603712","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Evaluation of NorESM-OC (versions 1 and 1.2), the ocean carbon-cycle stand-alone configuration of\nthe Norwegian Earth System Model (NorESM1)"}]},{"@id":"https://cir.nii.ac.jp/crid/1360588379385766400","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Global Carbon Budget 2024"}]},{"@id":"https://cir.nii.ac.jp/crid/1360588381062355584","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Insight into Combustion-Like Wear Processes Due to Unintended CO<sub>2</sub> and Nucleation-Mode Particle Emissions from Passenger Cars at Mild Brake Temperatures (>40 °C) under Realistic Driving Conditions"}]},{"@id":"https://cir.nii.ac.jp/crid/1360588381063518464","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Global upper ocean dissolved oxygen budget for constraining the biological carbon pump"}]},{"@id":"https://cir.nii.ac.jp/crid/1360845538932957312","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Rethinking the Causes of Deforestation: Lessons from Economic Models"}]},{"@id":"https://cir.nii.ac.jp/crid/1360853567704969984","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Role of tide-induced vertical mixing in the deep Pacific Ocean circulation"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855567860258688","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Substantial global carbon uptake by cement carbonation"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855567860641664","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Global fire emissions and the contribution of deforestation, savanna, forest, agricultural, and peat fires (1997–2009)"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855567862121984","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Oceanic sources, sinks, and transport of atmospheric CO<sub>2</sub>"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855567862171776","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Increase in observed net carbon dioxide uptake by land and oceans during the past 50 years"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855567862451584","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"On the Exchange of Momentum over the Open Ocean"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855567862538624","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"EDGAR v4.3.2 Global Atlas of the three major greenhouse gas emissions for the period 1970–2012"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855567864242432","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Global ocean storage of anthropogenic carbon"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855567864692736","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Net exchanges of CO<sub>2</sub>, CH<sub>4</sub>, and N<sub>2</sub>O between China's terrestrial ecosystems and the atmosphere and their contributions to global climate warming"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855567865077248","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Use of a process-based model for assessing the methane budgets of global terrestrial ecosystems and evaluation of uncertainty"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855567865603456","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Lower land-use emissions responsible for increased net land carbon sink during the slow warming period"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855567867224704","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Historical carbon dioxide emissions caused by land-use changes are possibly larger than assumed"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855567868377088","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Global Carbon Budget 2018"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855567869876736","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A Large and Persistent Carbon Sink in the World’s Forests"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855567870472064","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Carbon benefits of anthropogenic reactive nitrogen offset by nitrous oxide emissions"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855568613600128","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Spatiotemporal patterns of terrestrial carbon cycle during the 20th century"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855569490917120","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The decadal state of the terrestrial carbon cycle: Global retrievals of terrestrial carbon allocation, pools, and residence times"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855570135667200","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Rapid growth in CO2 emissions after the 2008–2009 global financial crisis"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855570506937984","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A dynamic global vegetation model for studies of the coupled atmosphere‐biosphere system"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855571317795200","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Agricultural and forestry trade drives large share of tropical deforestation emissions"}]},{"@id":"https://cir.nii.ac.jp/crid/1360857593682670848","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Climate Response to Emissions Reductions Due to COVID‐19: Initial Results From CovidMIP"}]},{"@id":"https://cir.nii.ac.jp/crid/1360857597319452800","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Net carbon emissions from African biosphere dominate pan-tropical atmospheric CO2 signal"}]},{"@id":"https://cir.nii.ac.jp/crid/1360857597399200768","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Global Emergence of Anthropogenic Climate Change in Fire Weather Indices"}]},{"@id":"https://cir.nii.ac.jp/crid/1360857598073381760","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The sensitivity of a depth-coordinate model to diapycnal mixing induced by practical implementations of the isopycnal tracer diffusion scheme"}]},{"@id":"https://cir.nii.ac.jp/crid/1360861291314583808","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The CarbonTracker Data Assimilation Shell (CTDAS) v1.0: implementation and global carbon balance 2001–2015"}]},{"@id":"https://cir.nii.ac.jp/crid/1360861293074968960","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Carbon Monitoring System Flux Net Biosphere Exchange 2020 (CMS-Flux NBE 2020)"}]},{"@id":"https://cir.nii.ac.jp/crid/1360861293088609408","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Forest carbon sink neutralized by pervasive growth-lifespan trade-offs"}]},{"@id":"https://cir.nii.ac.jp/crid/1360861711793733376","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Historical increases in land‐derived nutrient inputs may alleviate effects of a changing physical climate on the oceanic carbon cycle"}]},{"@id":"https://cir.nii.ac.jp/crid/1360861712063479808","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Bias in the attribution of forest carbon sinks"}]},{"@id":"https://cir.nii.ac.jp/crid/1360861712717995264","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Towards real-time verification of CO2 emissions"}]},{"@id":"https://cir.nii.ac.jp/crid/1360861713740531456","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Separating agricultural and non-agricultural fire seasonality at regional scales"}]},{"@id":"https://cir.nii.ac.jp/crid/1360861715108568192","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Reduction in greenhouse gas emissions from national climate legislation"}]},{"@id":"https://cir.nii.ac.jp/crid/1360861715164960256","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"On the impact of recent developments of the LMDz atmospheric general circulation model on the simulation of CO\n                    <sub>2</sub>\n                    transport"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865819382522752","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Consistency and Challenges in the Ocean Carbon Sink Estimate for the Global Carbon Budget"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865819382645248","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Contrasting projections of the ENSO-driven CO\n                    <sub>2</sub>\n                    flux variability in the equatorial Pacific under high-warming scenario"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865819396667136","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"How Well Do We Understand the Land‐Ocean‐Atmosphere Carbon Cycle?"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865819408048512","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The COVID-19 pandemic as an opportunity to weaken environmental protection in Brazil"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865819408229120","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Differences in land-based mitigation estimates reconciled by separating natural and land-use CO2 fluxes at the country level"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865819408369792","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Forest expansion dominates China’s land carbon sink since 1980"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865819408661632","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Sparse observations induce large biases in estimates of the global ocean CO\n            <sub>2</sub>\n            sink: an ocean model subsampling experiment"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865819409373824","@type":"Article","resourceType":"preprint","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Technical Note: The impact of industrial activity on the amount of atmospheric O\n                  <sub>2</sub>"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865819409374720","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Global and regional carbon budget for 2015–2020 inferred from OCO-2 based on an ensemble Kalman filter coupled with GEOS-Chem"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865819409379840","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Constraining ecosystem carbon dynamics in a data-limited world: integrating ecological \"common sense\" in a model–data fusion framework"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865819409381120","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Reconstructing European forest management from 1600 to 2010"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865819409384064","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"European anthropogenic AFOLU greenhouse gas emissions: a review and benchmark data"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865819409387648","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"CDIAC-FF: global and national CO\n                    <sub>2</sub>\n                    emissions from fossil fuel combustion and cement manufacture: 1751–2017"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865819409388672","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A 10-year global monthly averaged terrestrial net ecosystem exchange dataset inferred from the ACOS GOSAT v9 XCO\n                    <sub>2</sub>\n                    retrievals (GCAS2021)"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865819409390208","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"JULES-CN: a coupled terrestrial carbon–nitrogen scheme (JULES vn5.1)"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865819409392000","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Decadal climate predictions with the Canadian Earth System Model version 5 (CanESM5)"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865819409393280","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Improving the joint estimation of CO\n                    <sub>2</sub>\n                    and surface carbon fluxes using a constrained ensemble Kalman filter in COLA (v1.0)"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865819409394560","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Observation system simulation experiments in the Atlantic Ocean for enhanced surface ocean\n                    <i>p</i>\n                    CO\n                    <sub>2</sub>\n                    reconstructions"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865820392422144","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Oceanic CO\n                    <sub>2</sub>\n                    outgassing and biological production hotspots induced by pre-industrial river loads of nutrients and carbon in a global modeling approach"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865820405034752","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"An improved parameterization of leaf area index (LAI) seasonality in the Canadian Land Surface Scheme (CLASS) and Canadian Terrestrial Ecosystem Model (CTEM) modelling framework"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865820895563264","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Global and Regional Trends and Drivers of Fire Under Climate Change"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865821084302080","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Multiyear precipitation reduction strongly decreases carbon uptake over northern China"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865821084643328","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Constraint of satellite CO2 retrieval on the global carbon cycle from a Chinese atmospheric inversion system"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865821084649600","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Has global deforestation accelerated due to the COVID-19 pandemic?"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865821084794880","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Coronavirus, macroeconomy, and forests: What likely impacts?"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865821084926720","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Glossary"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865821085085056","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Estimation of Permafrost SOC Stock and Turnover Time Using a Land Surface Model With Vertical Heterogeneity of Permafrost Soils"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865821085086336","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Improved Quantification of Ocean Carbon Uptake by Using Machine Learning to Merge Global Models and pCO<sub>2</sub> Data"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865821085087488","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Inventorying Earth’s Land and Ocean Greenhouse Gases"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865821085089024","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Update on the Temperature Corrections of Global Air‐Sea CO<sub>2</sub> Flux Estimates"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865821085090688","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Sensitivity of the Global Ocean Carbon Sink to the Ocean Skin in a Climate Model"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865821085097088","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Stratification constrains future heat and carbon uptake in the Southern Ocean between 30°S and 55°S"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865821085436544","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The role of fire in global forest loss dynamics"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865821085471488","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Southern Ocean anthropogenic carbon sink constrained by sea surface salinity"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865821085534464","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Natural Variability and Anthropogenic Trends in the Ocean Carbon Sink"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865821085917568","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Modelled land use and land cover change emissions – a spatio-temporal comparison of different approaches"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865821085920128","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Reconstructions and predictions of the global carbon budget with an emission-driven Earth system model"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865821085921280","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Simulating the effect of tillage practices with the global  ecosystem model LPJmL (version 5.0-tillage)"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865821085922560","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Modelling the role of livestock grazing in C and N cycling in grasslands with LPJmL5.0-grazing"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865821937322112","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Changes in land use and management led to a decline in Eastern Europe’s terrestrial carbon sink"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865821941889408","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Carbon loss from forest degradation exceeds that from deforestation in the Brazilian Amazon"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137044848124416","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Global atmospheric CO\n                    <sub>2</sub>\n                    inverse models converging on neutral tropical land exchange, but disagreeing on fossil fuel and atmospheric growth rate"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137044859354752","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Predicting near-term variability in ocean carbon uptake"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137045747205376","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The dominant role of semi-arid ecosystems in the trend and variability of the land CO\n                    <sub>2</sub>\n                    sink"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418518431854080","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The community Noah land surface model with multiparameterization options (Noah-MP): 1. Model description and evaluation with local-scale measurements"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418518475126784","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Global energy growth is outpacing decarbonization"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418519008811008","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"CO<sub>2</sub> fertilization in temperate FACE experiments not representative of boreal and tropical forests"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418519617715328","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"PISCES-v2: an ocean biogeochemical model for carbon and ecosystem studies"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418519762953344","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Evaluation of CNRM Earth System Model, CNRM‐ESM2‐1: Role of Earth System Processes in Present‐Day and Future Climate"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418519858318848","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Carbon and nitrogen cycle dynamics in the O‐CN land surface model: 1. Model description, site‐scale evaluation, and sensitivity to parameter estimates"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418520815588736","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Sensitivity of atmospheric CO2 growth rate to observed changes in terrestrial water storage"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418520998776064","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Terrestrial carbon storage during the past 200 years: A Monte Carlo Analysis of CO<sub>2</sub> data from ice core and atmospheric measurements"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418521070642560","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Canadian Earth System Model version 5 (CanESM5.0.3)"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699993612432768","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Community Land Model Version 5: Description of New Features, Benchmarking, and Impact of Forcing Uncertainty"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699993774501376","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Implications of incorporating N cycling and N limitations on primary production in an individual-based dynamic vegetation model"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699994491926912","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Update on CO2 emissions"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699994726319616","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Natural and anthropogenic changes in atmospheric CO<sub>2</sub> over the last 1000 years from air in Antarctic ice and firn"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699995145375744","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Extension and integration of atmospheric carbon dioxide data into a globally consistent measurement record"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981468841427968","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A Bayesian ensemble data assimilation to constrain model parameters and land-use carbon emissions"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981470688457088","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Impacts of land cover and climate data selection on understanding terrestrial carbon dynamics and the CO\n                    <sub>2</sub>\n                    airborne fraction"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981470718863232","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Reconstruction of the history of anthropogenic CO2 concentrations in the ocean"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262943490782208","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"El Niño and a record CO2 rise"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262943529738496","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Effect of increasing CO\n                    <sub>2</sub>\n                    on the terrestrial carbon cycle"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262943782436352","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"<scp><scp>CO<sub>2</sub></scp></scp> emissions from land‐use change affected more by nitrogen cycle, than by the choice of land‐cover data"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262944749859584","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The DOE E3SM v1.1 Biogeochemistry Configuration: Description and Simulated Ecosystem‐Climate Responses to Historical Changes in Forcing"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262944774247168","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The global carbon budget 1959–2011"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262945374918656","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The gigatonne gap in China’s carbon dioxide inventories"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544419017750528","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Evaluation of 11 terrestrial carbon–nitrogen cycle models against observations from two temperate <scp>F</scp>ree‐<scp>A</scp>ir <scp>CO</scp><sub>2</sub><scp> E</scp>nrichment studies"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544419177955072","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Using the Fire Weather Index (FWI) to improve the estimation of fire emissions from fire radiative power (FRP) observations"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544419230972544","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Trends in the sources and sinks of carbon dioxide"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544420242659968","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Predicting the variable ocean carbon sink"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544420350135552","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"North American terrestrial CO2 uptake largely offset by CH4 and N2O emissions: toward a full accounting of the greenhouse gas budget"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544420444824704","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Relevance of methodological choices for accounting of land use change carbon fluxes"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544420865567744","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"LPJmL4 – a dynamic global vegetation model with managed land – Part 1: Model description"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544421076306944","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Saturation of the Southern Ocean CO\n                    <sub>2</sub>\n                    Sink Due to Recent Climate Change"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825893815030272","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Growth in emission transfers via international trade from 1990 to 2008"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825894636065536","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A comparison of estimates of global carbon dioxide emissions from fossil carbon sources"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825895915996800","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Persistent growth of CO2 emissions and implications for reaching climate targets"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825896156319360","@type":"Article","resourceType":"preprint","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Overview of the Coupled Model Intercomparison Project Phase 6 (CMIP6)  experimental design and organization"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107368373289216","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A METHOD FOR SCALING VEGETATION DYNAMICS: THE ECOSYSTEM DEMOGRAPHY MODEL (ED)"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107369201371648","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Constraining Projection-Based Estimates of the Future North Atlantic Carbon Uptake"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107369312397184","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Long-term decline of the Amazon carbon sink"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107369488360832","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Decadal predictions of the North Atlantic CO2 uptake"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107369500641920","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The International Land Model Benchmarking (ILAMB) System: Design, Theory, and Implementation"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107369518595840","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Persistent fossil fuel growth threatens the Paris Agreement and planetary health"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107370049765376","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Quantifying the Impact of Atmospheric Transport Uncertainty on CO<sub>2</sub> Surface Flux Estimates"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107370068841088","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Interannual sea–air CO\n                    <sub>2</sub>\n                    flux variability from an observation-driven ocean mixed-layer scheme"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388843385531520","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A new version of the CABLE land surface model (Subversion revision r4601) incorporating land use and land cover change, woody vegetation demography, and a novel optimisation-based approach to plant coordination of photosynthesis"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388844037300608","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The challenge to keep global warming below 2 °C"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388845430186624","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Biomass burning emissions estimated with a global fire assimilation system based on observed fire radiative power"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388845887028608","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The oceanic anthropogenic CO<sub>2</sub> sink: Storage, air‐sea fluxes, and transports over the industrial era"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388845903289344","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The collection 6 MODIS active fire detection algorithm and fire products"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670318429761664","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Global Carbon Budget 2020"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670318624808832","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Sensitivity of tropical carbon to climate change constrained by carbon dioxide variability"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670318691980032","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"High predictability of terrestrial carbon fluxes from an initialized decadal prediction system"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670319061030528","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Implementing the nitrogen cycle into the dynamic global vegetation, hydrology, and crop growth model LPJmL (version 5.0)"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670319182085760","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"21st Century drought-related fires counteract the decline of Amazon deforestation carbon emissions"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670319527437184","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Carbon and Other Biogeochemical Cycles"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670319747368704","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Carbon dioxide emissions continue to grow amidst slowly emerging climate policies"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670320123808512","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Audit of the global carbon budget: estimate errors and their impact on uptake uncertainty"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670320332220928","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Rates of change in natural and anthropogenic radiative forcing over the past 20,000 years"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670320363671040","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Vegetation dynamics – simulating responses to climatic change"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951794882562176","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"UKESM1: Description and Evaluation of the U.K. Earth System Model"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951795363425792","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Projected land photosynthesis constrained by changes in the seasonal cycle of atmospheric CO2"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951795479774080","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Carbon emissions from land use and land-cover change"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951795538424704","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The carbon cycle in the Australian Community Climate and Earth System Simulator (ACCESS-ESM1) – Part 1: Model description and pre-industrial simulation"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233269606865152","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Studies of Recent Changes in Atmospheric O2 Content"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233270064048768","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Presentation and Evaluation of the IPSL‐CM6A‐LR Climate Model"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233270222144768","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Developments in the MPI‐M Earth System Model version 1.2 (MPI‐ESM1.2) and Its Response to Increasing CO<sub>2</sub>"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233270341205248","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Testing global ocean carbon cycle models using measurements of atmospheric O<sub>2</sub> and CO<sub>2</sub> concentration"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233270585874176","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Revision of global carbon fluxes based on a reassessment of oceanic and riverine carbon transport"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233270755810816","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Global Carbon Budget 2017"}]},{"@id":"https://cir.nii.ac.jp/crid/1390583934062442624","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Role of Harvested Wood Products in Meeting Long-term Climate Targets for China"}]},{"@id":"https://cir.nii.ac.jp/crid/1523106605858309888","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Global trends of ocean CO₂ sink and ocean acidification : an observation-based reconstruction of surface ocean inorganic carbon variables"}]},{"@id":"https://cir.nii.ac.jp/crid/1573105974831354496","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Climatological mean and decadal change in surface ocean pCO_2, and net sea-air CO_2 flux over the global oceans"}]},{"@id":"https://cir.nii.ac.jp/crid/1882553967472426368","@type":"Dataset","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Gridded fossil CO2 emissions and related O2 combustion consistent with national inventories"}]},{"@id":"https://cir.nii.ac.jp/crid/1884242817348662400","@type":"Dataset","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Gridded fossil CO2 emissions and related O2 combustion consistent with national inventories 1959-2018"}]},{"@id":"https://cir.nii.ac.jp/crid/2050588892112938112","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Toward a long-term atmospheric CO2 inversion for elucidating natural carbon fluxes : technical notes of NISMON-CO2 v2021.1"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.5194/essd-15-5301-2023"},{"@type":"KAKEN","@value":"PRODUCT-25307580"},{"@type":"OPENAIRE","@value":"doi_dedup___::d98241b5f2d5f5c33e3444e10ab0e85e"},{"@type":"CROSSREF","@value":"10.1016/j.jag.2024.104117_references_DOI_6rhY5mUVGbq3cJV3EmpJ7UnOabM"},{"@type":"CROSSREF","@value":"10.1007/s11631-024-00735-w_references_DOI_6rhY5mUVGbq3cJV3EmpJ7UnOabM"},{"@type":"CROSSREF","@value":"10.5194/essd-17-3807-2025_references_DOI_6rhY5mUVGbq3cJV3EmpJ7UnOabM"},{"@type":"CROSSREF","@value":"10.1038/s41467-024-46101-5_references_DOI_6rhY5mUVGbq3cJV3EmpJ7UnOabM"},{"@type":"CROSSREF","@value":"10.1038/s41597-024-03316-x_references_DOI_6rhY5mUVGbq3cJV3EmpJ7UnOabM"},{"@type":"CROSSREF","@value":"10.1057/s41278-024-00307-y_references_DOI_6rhY5mUVGbq3cJV3EmpJ7UnOabM"},{"@type":"CROSSREF","@value":"10.3390/min14090876_references_DOI_6rhY5mUVGbq3cJV3EmpJ7UnOabM"},{"@type":"CROSSREF","@value":"10.15684/formath.23.003_references_DOI_6rhY5mUVGbq3cJV3EmpJ7UnOabM"},{"@type":"CROSSREF","@value":"10.5194/essd-15-5301-2023_references_DOI_6rhY5mUVGbq3cJV3EmpJ7UnOabM"},{"@type":"CROSSREF","@value":"10.5194/essd-17-965-2025_references_DOI_6rhY5mUVGbq3cJV3EmpJ7UnOabM"},{"@type":"CROSSREF","@value":"10.1021/acsestair.4c00350_references_DOI_6rhY5mUVGbq3cJV3EmpJ7UnOabM"},{"@type":"CROSSREF","@value":"10.1038/s43247-024-01886-7_references_DOI_6rhY5mUVGbq3cJV3EmpJ7UnOabM"}]}