{"@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/1360002214351123328.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1002/2016wr019267"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2016WR019267"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/pdf/10.1002/2016WR019267"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/full-xml/10.1002/2016WR019267"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2016WR019267"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Differences in behavior and distribution of permafrost‐related lakes in <scp>C</scp>entral <scp>Y</scp>akutia and their response to climatic drivers"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>The Central Yakutian permafrost landscape is rapidly being modified by land use and global warming, but small‐scale thermokarst process variability and hydrological conditions are poorly understood. We analyze lake‐area changes and thaw subsidence of young thermokarst lakes on ice‐complex deposits (yedoma lakes) in comparison to residual lakes in alas basins during the last 70 years for a local study site and we record regional lake size and distribution on different ice‐rich permafrost terraces using satellite and historical airborne imagery. Statistical analysis of climatic and ground‐temperature data identified driving factors of yedoma‐ and alas‐lake changes. Overall, lake area is larger today than in 1944 but alas‐lake levels have oscillated greatly over 70 years, with a mean alas‐lake‐radius change rate of 1.6 ± 3.0 m/yr. Anthropogenic disturbance and forest degradation initiated, and climate forced rapid, continuous yedoma‐lake growth. The mean yedoma lake‐radius change rate equals 1.2 ± 1.0 m/yr over the whole observation period. Mean thaw subsidence below yedoma lakes is 6.2 ± 1.4 cm/yr. Multiple regression analysis suggests that winter precipitation, winter temperature, and active‐layer properties are primary controllers of area changes in both lake types; summer weather and permafrost conditions additionally influence yedoma‐lake growth rates. The main controlling factors of alas‐lake changes are unclear due to larger catchment areas and subsurface hydrological conditions. Increasing thermokarst activity is currently linked to older terraces with higher ground‐ice contents, but thermokarst activity will likely stay high and wet conditions will persist within the near future in Central Yakutian alas basins.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380002214351123586","@type":"Researcher","foaf:name":[{"@value":"M. Ulrich"}],"jpcoar:affiliationName":[{"@value":"Institute for Geography, Leipzig University Leipzig Germany"}]},{"@id":"https://cir.nii.ac.jp/crid/1380002214351123584","@type":"Researcher","foaf:name":[{"@value":"H. Matthes"}],"jpcoar:affiliationName":[{"@value":"Atmospheric Circulations Section Alfred Wegener Institute Potsdam Germany"}]},{"@id":"https://cir.nii.ac.jp/crid/1380002214351123585","@type":"Researcher","foaf:name":[{"@value":"L. Schirrmeister"}],"jpcoar:affiliationName":[{"@value":"Periglacial Research Section Alfred Wegener Institute Potsdam Germany"}]},{"@id":"https://cir.nii.ac.jp/crid/1380003442469468801","@type":"Researcher","foaf:name":[{"@value":"J. Schütze"}],"jpcoar:affiliationName":[{"@value":"Department of Fundamental Science University of Applied Sciences Jena Jena Germany"}]},{"@id":"https://cir.nii.ac.jp/crid/1380002214351123328","@type":"Researcher","foaf:name":[{"@value":"H. Park"}],"jpcoar:affiliationName":[{"@value":"Institute of Arctic Climate and Environment Research, Japan Agency for Marine‐Earth Science and Technology Yokosuka Japan"},{"@value":"Institute for Space‐Earth Environmental Research, Nagoya University Nagoya Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380003442469468800","@type":"Researcher","foaf:name":[{"@value":"Y. Iijima"}],"jpcoar:affiliationName":[{"@value":"Graduate School of Bioresources Mie University Tsu Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380002214351123456","@type":"Researcher","foaf:name":[{"@value":"A. N. Fedorov"}],"jpcoar:affiliationName":[{"@value":"Melnikov Permafrost Institute, SB RAS Yakutsk Russia"},{"@value":"Faculty of Geology and Survey, North‐Eastern Federal University Yakutsk Russia"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00431397"},{"@type":"EISSN","@value":"19447973"}],"prism:publicationName":[{"@value":"Water Resources Research"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2017-02","prism:volume":"53","prism:number":"2","prism:startingPage":"1167","prism:endingPage":"1188"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2016WR019267"},{"@id":"https://onlinelibrary.wiley.com/doi/pdf/10.1002/2016WR019267"},{"@id":"https://onlinelibrary.wiley.com/doi/full-xml/10.1002/2016WR019267"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2016WR019267"}],"createdAt":"2017-01-10","modifiedAt":"2023-09-01","project":[{"@id":"https://cir.nii.ac.jp/crid/1040000781967350016","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"17K08019"},{"@type":"JGN","@value":"JP17K08019"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-17K08019/"}],"notation":[{"@language":"ja","@value":"永久凍土地域の森林土壌は将来湿潤化するか？"},{"@language":"en","@value":"A modeling study on forest soil moisture in the permafrost region under future climate conditions: wet or dry?"}]},{"@id":"https://cir.nii.ac.jp/crid/1040282257268254336","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"26340018"},{"@type":"JGN","@value":"JP26340018"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-26340018/"}],"notation":[{"@language":"ja","@value":"北方河川流出量は海氷減少に影響している"},{"@language":"en","@value":"Assessing influences of river discharge on declining Arctic sea ice"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360001113991970944","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Shrinking ponds in subarctic Alaska based on 1950–2002 remotely sensed images"}]},{"@id":"https://cir.nii.ac.jp/crid/1360001114007829760","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Contemporary (1951–2001) Evolution of Lakes in the Old Crow Basin, Northern Yukon, Canada: Remote Sensing, Numerical Modeling, and Stable Isotope Analysis"}]},{"@id":"https://cir.nii.ac.jp/crid/1360001114007918976","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Methane emissions from permafrost thaw lakes limited by lake drainage"}]},{"@id":"https://cir.nii.ac.jp/crid/1360001114008047872","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Tundra lake changes from 1978 to 2001 on the Tuktoyaktuk Peninsula, western Canadian Arctic"}]},{"@id":"https://cir.nii.ac.jp/crid/1360001114183053056","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Origin and polycyclic behaviour of tundra thaw slumps, Mackenzie Delta region, Northwest Territories, Canada"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002214534737280","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Sap flow changes in relation to permafrost degradation under increasing precipitation in an eastern Siberian larch forest"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002214596068352","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Enhancement of Arctic storm activity in relation to permafrost degradation in eastern Siberia"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004239515825920","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Thermokarst Development Detected from High-Definition Topographic Data in Central Yakutia"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011145378391296","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The application of a coupled hydrological and biogeochemical model (CHANGE) for modeling of energy, water, and CO<sub>2</sub>exchanges over a larch forest in eastern Siberia"}]},{"@id":"https://cir.nii.ac.jp/crid/1360017279830020480","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Ground Surface Displacement After a Forest Fire Near Mayya, Eastern Siberia, Using InSAR: Observation and Implication for Geophysical Modeling"}]},{"@id":"https://cir.nii.ac.jp/crid/1360282588984310912","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Thermokarst Lakes as a Source of Atmospheric CH\n                    <sub>4</sub>\n                    During the Last Deglaciation"}]},{"@id":"https://cir.nii.ac.jp/crid/1360282588984649344","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The transient layer: implications for geocryology and climate‐change science"}]},{"@id":"https://cir.nii.ac.jp/crid/1360282589150439680","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"8.21 Thermokarst Lakes, Drainage, and Drained Basins"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292619558124416","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Evolution of the banks of thermokarst lakes in Central Yakutia (Central Siberia) due to retrogressive thaw slump activity controlled by insolation"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292620823792000","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Modern thermokarst lake dynamics in the continuous permafrost zone, northern Seward Peninsula, Alaska"}]},{"@id":"https://cir.nii.ac.jp/crid/1360298345005785216","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Contribution of summer net precipitation to winter river discharge in permafrost zone of the Lena River basin"}]},{"@id":"https://cir.nii.ac.jp/crid/1360564063961137536","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Spatial and temporal variability in active layer thickness over the Russian Arctic drainage basin"}]},{"@id":"https://cir.nii.ac.jp/crid/1360564063961298048","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Abrupt increases in soil temperatures following increased precipitation in a permafrost region, central Lena River basin, Russia"}]},{"@id":"https://cir.nii.ac.jp/crid/1360564064127384832","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Spatial analyses of thermokarst lakes and basins in Yedoma landscapes of the Lena Delta"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574095671970816","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Interannual variations in the areas of thermokarst lakes in Central Yakutia"}]},{"@id":"https://cir.nii.ac.jp/crid/1360579819987992448","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Thermokarst Landscape Development Detected by Multiple-Geospatial Data in Churapcha, Eastern Siberia"}]},{"@id":"https://cir.nii.ac.jp/crid/1360845538923653376","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Estimating the water balance of a thermokarst lake in the middle of the Lena River basin, eastern Siberia"}]},{"@id":"https://cir.nii.ac.jp/crid/1360845538938271744","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Satellite-derived changes in the permafrost landscape of central Yakutia, 2000–2011: Wetting, drying, and fires"}]},{"@id":"https://cir.nii.ac.jp/crid/1360845539103768064","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Thermokarst Lake Morphometry and Erosion Features in Two Peat Plateau Areas of Northeast European Russia"}]},{"@id":"https://cir.nii.ac.jp/crid/1360845539103874432","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Simulating the decadal‐ to millennial‐scale dynamics of morphology and sequestered carbon mobilization of two thermokarst lakes in NW Alaska"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846640725538432","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Permafrost livelihoods: A transdisciplinary review and analysis of thermokarst-based systems of indigenous land use"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846641055021568","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Recent air temperature changes in the permafrost landscapes of northeastern Eurasia"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855570185108736","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"CH<sub>4</sub>emission from different stages of thermokarst formation in Central Yakutia, East Siberia"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855570508967680","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Arctic Lake Physical Processes and Regimes with Implications for Winter Water Availability and Management in the National Petroleum Reserve Alaska"}]},{"@id":"https://cir.nii.ac.jp/crid/1360861704770300416","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Numerical Assessments of Excess Ice Impacts on Permafrost and Greenhouse Gases in a Siberian Tundra Site Under a Warming Climate"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137043689495296","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Thermokarst in Siberian ice‐rich permafrost: Comparison to asymmetric scalloped depressions on Mars"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137045449310720","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Depth, ice thickness, and ice‐out timing cause divergent hydrologic responses among Arctic lakes"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418518553237120","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Landsat-based mapping of thermokarst lake dynamics on the Tuktoyaktuk Coastal Plain, Northwest Territories, Canada since 1985"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418518650169344","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A Political Ecology of “Water in Mind”: Attributing Perceptions in the Era of Global Climate Change"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418519586135808","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Thermokarst rates intensify due to climate change and forest fragmentation in an Alaskan boreal forest lowland"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418521418743808","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Time‐dependent morphology of thaw lakes and taliks in deep and shallow ground ice"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699995213945344","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The <I>Alaas:</I> Cattle Economy and Environmental Perception of Sedentary Sakhas in Central Yakutia"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981469304583552","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Temporal and spatial pattern of thermokarst lake area changes at Yukon Flats, Alaska"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262943840395392","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Mechanisms influencing changes in lake area in Alaskan boreal forest"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544420403369984","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Shrinking thermokarst ponds and groundwater dynamics in discontinuous permafrost near council, Alaska"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544420854719872","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Summary of current radiometric calibration coefficients for Landsat MSS, TM, ETM+, and EO-1 ALI sensors"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825895806654464","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Response of permafrost landscapes of Central Yakutia to current changes of climate, and anthropogenic impacts"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107369337132416","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Disappearing Arctic Lakes"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107370831651712","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A new procedure for gridding elevation and stream line data with automatic removal of spurious pits"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388844751235072","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Arctic terrestrial hydrology: A synthesis of processes, regional effects, and research challenges"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388845438578816","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Changes in lake area in response to thermokarst processes and climate in Old Crow Flats, Yukon"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388845974718720","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Thermokarst as a short‐term permafrost disturbance, Central Yakutia"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670320971483392","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Water Body Distributions Across Scales: A Remote Sensing Based Comparison of Three Arctic Tundra Wetlands"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951793245999744","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Impact of the timing and duration of seasonal snow cover on the active layer and permafrost in the Alaskan Arctic"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951793555201664","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Influence of forest clear‐cutting on the thermal and hydrological regime of the active layer near Yakutsk, eastern Siberia"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951794422366976","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Present-day variability and Holocene dynamics of permafrost-affected lakes in central Yakutia (Eastern Siberia) inferred from diatom records"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951794529333376","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Gone the Bull of Winter?"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951795310805376","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Past and recent changes in air and permafrost temperatures in eastern Siberia"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233268963221120","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Modification of normalised difference water index (NDWI) to enhance open water features in remotely sensed imagery"}]},{"@id":"https://cir.nii.ac.jp/crid/1370002214351123463","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The dynamics of thermokarst lakes under climate changes since 1950, Central Yakutia"}]},{"@id":"https://cir.nii.ac.jp/crid/1370002214351123476","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The vegetation of Central Yakutian alases, Folia Geobot"}]},{"@id":"https://cir.nii.ac.jp/crid/1370002214351123588","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Cyclic variations in the water level of alas lakes in Central Yakutia and their relation to climate element variations (in Russian)"}]},{"@id":"https://cir.nii.ac.jp/crid/1370002214351123592","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Changes in thermokarst lake sizes in different regions of Russia for the last 30 years [in Russian]"}]},{"@id":"https://cir.nii.ac.jp/crid/1570854175159530112","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Thermokarst phenomena and land-forms due to frost heaving in Central Yakutia"}]},{"@id":"https://cir.nii.ac.jp/crid/2051996266981883776","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Surface displacement revealed by L-band InSAR analysis in the Mayya area, Central Yakutia, underlain by continuous permafrost"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1002/2016wr019267"},{"@type":"KAKEN","@value":"PRODUCT-21483089"},{"@type":"KAKEN","@value":"PRODUCT-21054016"},{"@type":"OPENAIRE","@value":"doi_dedup___::2c026a2ab7a95221ddaf2aa079b0b709"},{"@type":"CROSSREF","@value":"10.3390/rs10101579_references_DOI_NXxckgZKauJ4WPLnf1HDXI9g3PR"},{"@type":"CROSSREF","@value":"10.1029/2022ea002476_references_DOI_NXxckgZKauJ4WPLnf1HDXI9g3PR"},{"@type":"CROSSREF","@value":"10.1016/j.ancene.2017.06.001_references_DOI_NXxckgZKauJ4WPLnf1HDXI9g3PR"},{"@type":"CROSSREF","@value":"10.1016/j.jhydrol.2022.128797_references_DOI_NXxckgZKauJ4WPLnf1HDXI9g3PR"},{"@type":"CROSSREF","@value":"10.3389/feart.2021.750298_references_DOI_No2BrOwixIghCj9QoJPRdJXpmJ7"},{"@type":"CROSSREF","@value":"10.1186/s40623-020-01266-3_references_DOI_NXxckgZKauJ4WPLnf1HDXI9g3PR"},{"@type":"CROSSREF","@value":"10.3389/feart.2021.704447_references_DOI_NXxckgZKauJ4WPLnf1HDXI9g3PR"}]}