{"created":"2023-07-25T11:11:27.741915+00:00","id":16015,"links":{},"metadata":{"_buckets":{"deposit":"f2958730-190d-48ed-b6eb-0ae559e5c8ce"},"_deposit":{"created_by":26,"id":"16015","owners":[26],"pid":{"revision_id":0,"type":"depid","value":"16015"},"status":"published"},"_oai":{"id":"oai:nipr.repo.nii.ac.jp:00016015","sets":["1259:1267:2014"]},"author_link":["70274","70275","70277","70276"],"item_10001_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2020-06","bibliographicIssueDateType":"Issued"},"bibliographicPageStart":"100525","bibliographicVolumeNumber":"24","bibliographic_titles":[{},{"bibliographic_title":"Polar Science","bibliographic_titleLang":"en"}]}]},"item_10001_description_5":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"Global climate closely links with the Arctic Ocean ecosystem especially in the Barents Sea. The distributions and correlations among chlorophyll-a (CHL), sea ice concentration (ICE), wind speed (WIND), sea surface temperature (SST) and mixed layer depth (MLD) are studied within the region of Barents Sea (70°N-80°N, 30°E−40°E) over the period 2003–2013. CHL increased from north to south in general. Ice melted rapidly in the southern region (70°N-75°N) and had less impact than SST on phytoplankton blooming. Melting ice in northern region (75°N-80°N) contributed significant source on phytoplankton development. WIND had negative correlations with CHL in spring blooming season and had positive correlations during autumn. \nDimethylsulfide (DMS) concentration and sea-to-air DMS flux are simulated using a comprehensive biogeochemical model. The key model parameters are calibrated using a genetic algorithm under contemporary climate conditions. Environmental factors and DMS sea-air flux are compared for 1CO2 and 4CO2 climate conditions. By 4CO2, SST increases more than doubles, DMS increases 27.5%. Mean annual DMS sea-to-air flux increases 323%. The increase of DMS flux under 4CO2 conditions indicates that Arctic climate may be counteracting with the warming by 4CO2.","subitem_description_type":"Abstract"}]},"item_10001_relation_14":{"attribute_name":"DOI","attribute_value_mlt":[{"subitem_relation_name":[{"subitem_relation_name_text":"10.1016/j.polar.2020.100525"}],"subitem_relation_type_id":{"subitem_relation_type_id_text":"https://doi.org/10.1016/j.polar.2020.100525","subitem_relation_type_select":"DOI"}}]},"item_10001_source_id_9":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"18739652","subitem_source_identifier_type":"ISSN"}]},"item_access_right":{"attribute_name":"アクセス権","attribute_value_mlt":[{"subitem_access_right":"metadata only access","subitem_access_right_uri":"http://purl.org/coar/access_right/c_14cb"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"Qu, Bo","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Gabric, Albert J.","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Zeng, Meifang","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Liu, Xiao","creatorNameLang":"en"}],"nameIdentifiers":[{}]}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"Dimethylsulfide","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"Chlorophyll","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"Sea ice concentration","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"Wind speed","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"Barents Sea","subitem_subject_language":"en","subitem_subject_scheme":"Other"}]},"item_language":{"attribute_name":"言語","attribute_value_mlt":[{"subitem_language":"eng"}]},"item_resource_type":{"attribute_name":"資源タイプ","attribute_value_mlt":[{"resourcetype":"journal article","resourceuri":"http://purl.org/coar/resource_type/c_6501"}]},"item_title":"Correlations among phytoplankton biomass, sea ice and wind speed in Barents Sea and the future climate trends","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"Correlations among phytoplankton biomass, sea ice and wind speed in Barents Sea and the future climate trends"},{"subitem_title":"Correlations among phytoplankton biomass, sea ice and wind speed in Barents Sea and the future climate trends","subitem_title_language":"en"}]},"item_type_id":"10001","owner":"26","path":["2014"],"pubdate":{"attribute_name":"公開日","attribute_value":"2020-06-24"},"publish_date":"2020-06-24","publish_status":"0","recid":"16015","relation_version_is_last":true,"title":["Correlations among phytoplankton biomass, sea ice and wind speed in Barents Sea and the future climate trends"],"weko_creator_id":"26","weko_shared_id":-1},"updated":"2023-07-25T13:00:45.248820+00:00"}