{"@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/1360002214596068352.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1002/joc.4629"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjoc.4629"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/full/10.1002/joc.4629"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Enhancement of Arctic storm activity in relation to permafrost degradation in eastern Siberia"}],"dcterms:alternative":[{"@value":"ARCTIC STORM ACTIVITY IN RELATION TO PERMAFROST DEGRADATION"}],"description":[{"notation":[{"@value":"In the last decade, increases in both soil temperature and active layer thickness have been observed in the central Lena River basin, an area located in the centre of continuous permafrost in the Eurasian continent. Increased soil temperatures have been accompanied by corresponding increases in soil moisture within the active layer at many sites throughout the region. These underground hydro-thermal changes are believed to be primarily due to perennially wet climate conditions, rather than the atmospheric warming alone that has resulted in abnormally large amounts of winter snow accumulation and late summer rainfall in the Lena River basin. This study aimed to clarify the linkage between atmospheric and land surface variations in regions of continuous permafrost in eastern Siberia based on in situ observation and atmospheric climatic data analyses. These wet conditions in 2004–2008 were likely caused by the enhancement of cyclones over the Arctic Ocean and eastward propagation of storm activity during late summer and early winter. Water vapour flux was enhanced in conjunction with the manifestation of precipitation in eastern Siberia. As a result, consecutive positive anomalies of winter snow accumulation and precipitation during the subsequent summers effectively humidified land surfaces in the permafrost region from 2005 onwards, which resulted in abrupt soil warming and wetting of both the active layer and the upper part of the permafrost. The positive effects on increasing soil temperatures of both snowfall in winter and rainfall in summer have been observed in eastern Siberia since the 1990s, and have also been demonstrated through land surface simulation. Results of these hydro-climatic changes indicated that the near-surface permafrost in eastern Siberia is vulnerable to the climatic conditions that have arisen due to the acceleration of the hydrological cycle that has resulted from the aforementioned period of warming."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1420564276167292800","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"80392934"},{"@type":"NRID","@value":"1000080392934"},{"@type":"ORCID","@value":"0000-0003-0590-5696"},{"@type":"CINII_AUTHOR_ID","@value":"DA19554835"},{"@type":"URI","@value":"https://ci.nii.ac.jp/author/DA19554835#entity"},{"@type":"URI","@value":"https://viaf.org/viaf/NII%7CDA19554835"},{"@type":"NRID","@value":"9000002496765"},{"@type":"NRID","@value":"9000002646073"},{"@type":"NRID","@value":"9000258490522"},{"@type":"NRID","@value":"9000004079243"},{"@type":"NRID","@value":"9000270174988"},{"@type":"NRID","@value":"9000365043257"},{"@type":"NRID","@value":"9000006280364"},{"@type":"NRID","@value":"9000020066745"},{"@type":"NRID","@value":"9000004072874"},{"@type":"NRID","@value":"9000380122999"},{"@type":"NRID","@value":"9000413547015"},{"@type":"NRID","@value":"9000006512866"},{"@type":"NRID","@value":"9000409333938"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/yshriijima"}],"foaf:name":[{"@value":"Yoshihiro 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Tachibana"}],"jpcoar:affiliationName":[{"@value":"Climate and Ecosystem Dynamics Division; Mie University; Tsu Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380566392677195523","@type":"Researcher","foaf:name":[{"@value":"Alexander N. Fedorov"}],"jpcoar:affiliationName":[{"@value":"Cryogenic Landscape Laboratory; Melnikov Permafrost Institute, SB RAS; Yakutsk Russia"},{"@value":"International Centre BEST; North-Eastern Federal University; Yakutsk Russia"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"08998418"}],"prism:publicationName":[{"@value":"International Journal of Climatology"}],"dc:publisher":[{"@value":"Wiley"}],"prism:publicationDate":"2016-02-03","prism:volume":"36","prism:number":"13","prism:startingPage":"4265","prism:endingPage":"4275"},"reviewed":"false","dc:rights":["http://doi.wiley.com/10.1002/tdm_license_1","http://onlinelibrary.wiley.com/termsAndConditions"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjoc.4629"},{"@id":"https://onlinelibrary.wiley.com/doi/full/10.1002/joc.4629"}],"createdAt":"2016-02-03","modifiedAt":"2021-07-05","project":[{"@id":"https://cir.nii.ac.jp/crid/1040000782192375296","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"24241009"},{"@type":"JGN","@value":"JP24241009"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-24241009/"}],"notation":[{"@language":"ja","@value":"北極の温暖化増幅における季節サイクルと多圏相互作用の追究"},{"@language":"en","@value":"Understanding the seasonal cycle and multiple intercations related to the Arctic amplification"}]},{"@id":"https://cir.nii.ac.jp/crid/1040282256896818432","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"16K13880"},{"@type":"JGN","@value":"JP16K13880"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-16K13880/"}],"notation":[{"@language":"ja","@value":"北極振動と南極振動の「メタ・テレコネクション」～両半球をつなぐ航路は何か～"},{"@language":"en","@value":"Interhemispheric Synchronization Between the AO and the AAO"}]},{"@id":"https://cir.nii.ac.jp/crid/1040282257078313728","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"22106001"},{"@type":"JGN","@value":"JP22106001"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-ORGANIZER-22106001/"}],"notation":[{"@language":"ja","@value":"中緯度大気海洋結合系研究の推進と統括"},{"@language":"en","@value":"Promotion and Supervision of the \"Hot Spot Project\" on the Extratropical Ocean-Atmosphere Coupled System"}]},{"@id":"https://cir.nii.ac.jp/crid/1040282257213120768","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"25220201"},{"@type":"JGN","@value":"JP25220201"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-25220201/"}],"notation":[{"@language":"ja","@value":"乾燥地災害学の体系化"},{"@language":"en","@value":"Integrating dryland disaster science"}]},{"@id":"https://cir.nii.ac.jp/crid/1040282257257796864","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"26242026"},{"@type":"JGN","@value":"JP26242026"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-26242026/"}],"notation":[{"@language":"ja","@value":"植生景観構造を考慮した東ユーラシア永久凍土変化の広域評価"},{"@language":"en","@value":"Permafrost mapping under changing environment in eastern Eurasia"}]},{"@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/1050301927790445952","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Effect of snow cover on pan-Arctic permafrost thermal regimes"}]},{"@id":"https://cir.nii.ac.jp/crid/1050864877743867264","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"An observation-based assessment of the influences of air temperature and snow depth on soil 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