{"created":"2023-07-25T11:07:13.811812+00:00","id":10921,"links":{},"metadata":{"_buckets":{"deposit":"4e251f2a-09e6-49ad-8717-063b51b0ec85"},"_deposit":{"created_by":27,"id":"10921","owners":[27],"pid":{"revision_id":0,"type":"depid","value":"10921"},"status":"published"},"_oai":{"id":"oai:nipr.repo.nii.ac.jp:00010921","sets":[]},"author_link":["23699","23697","23698"],"item_10001_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2015-09","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"3","bibliographicPageEnd":"292","bibliographicPageStart":"277","bibliographicVolumeNumber":"9","bibliographic_titles":[{"bibliographic_title":" Polar Science  "},{"bibliographic_title":" Polar Science  ","bibliographic_titleLang":"en"}]}]},"item_10001_description_5":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"Future changes in precipitation intensity over the Arctic were calculated based on three-member ensemble simulations using a global atmospheric model with a high horizontal resolution (60-km grid) for the period 1872–2099 (228 years). During 1872–2005, the model was forced with observed historical sea surface temperature (SST) data, while during 2006–2099, boundary SST data were estimated using the multi-model ensemble (MME) of the Coupled Model Intercomparison Project, Phase 3 (CMIP3) model, assuming the A1B emission scenario. The annual mean precipitation (PAVE), the simple daily precipitation intensity index (SDII), and the maximum 5-day precipitation total (R5d) averaged over the Arctic increased monotonically towards the end of the 21st century. Over the Arctic, the conversion rate from water vapor to precipitation per one degree temperature increase is larger for PAVE than for R5d, which is opposite to the tropics and mid-latitudes. The increases in PAVE, SDII, and R5d can be partly attributed to an increase in water vapor associated with increasing temperatures, and to an increase in the horizontal transport of water vapor from low to high latitudes associated with transient eddies.","subitem_description_type":"Abstract"}]},"item_10001_description_6":{"attribute_name":"内容記述","attribute_value_mlt":[{"subitem_description":"1872年から2099年の228年間について水平方向に高解像度の全球大気モデル（60㎞格子）の3つの実験に基づき、北極圏の降水強度の将来変化を計算した。1872年から2005年の期間は観測された海面水温をモデルに与え、2006年から2099年の期間は第３期結合モデル国際相互比較計画の複数のモデルによるA1B排出シナリオ実験から海面水温を推定値した。北極圏における年均降水量(PAVE)、単純日降水強度指数(SDII)、最大5日積算降水量(R5d)は21世紀末に向けて単調に増加する。北極圏では、気温の1度上昇当たりの水蒸気から降水への変換効率は、PAVEのほうがR5dより大きく、これは熱帯と中緯度と逆である。PAVE、SDII、R5dの増加は、気温の上昇に伴う水蒸気の増加、および非定常渦に伴う低緯度から高緯度への水蒸気の水平輸送の増加に起因する","subitem_description_type":"Other"}]},"item_10001_relation_14":{"attribute_name":"DOI","attribute_value_mlt":[{"subitem_relation_name":[{"subitem_relation_name_text":"10.1016/j.polar.2015.08.001"}],"subitem_relation_type_id":{"subitem_relation_type_id_text":"http://doi.org/10.1016/j.polar.2015.08.001","subitem_relation_type_select":"DOI"}}]},"item_10001_source_id_9":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"1873-9652 ","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":"Kusunoki, Shoji ","creatorNameLang":"en"}],"nameIdentifiers":[{"nameIdentifier":"23697","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"Mizuta, Ryo ","creatorNameLang":"en"}],"nameIdentifiers":[{"nameIdentifier":"23698","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"Hosaka, Masahiro ","creatorNameLang":"en"}],"nameIdentifiers":[{"nameIdentifier":"23699","nameIdentifierScheme":"WEKO"}]}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"The Arctic","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"Precipitation intensity","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"Polar amplification","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"Global atmospheric model","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"Water vapor transport","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":"Future changes in precipitation intensity over the Arctic projected by a global atmospheric model with a 60-km grid size","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"Future changes in precipitation intensity over the Arctic projected by a global atmospheric model with a 60-km grid size"},{"subitem_title":"Future changes in precipitation intensity over the Arctic projected by a global atmospheric model with a 60-km grid size","subitem_title_language":"en"}]},"item_type_id":"10001","owner":"27","path":["1448"],"pubdate":{"attribute_name":"公開日","attribute_value":"2015-09-03"},"publish_date":"2015-09-03","publish_status":"0","recid":"10921","relation_version_is_last":true,"title":["Future changes in precipitation intensity over the Arctic projected by a global atmospheric model with a 60-km grid size"],"weko_creator_id":"27","weko_shared_id":27},"updated":"2023-07-25T16:22:43.720206+00:00"}