{"created":"2023-07-25T09:03:14.294383+00:00","id":852,"links":{},"metadata":{"_buckets":{"deposit":"991fa636-2e58-409d-bb00-a66bf12a1e0b"},"_deposit":{"created_by":3,"id":"852","owners":[3],"pid":{"revision_id":0,"type":"depid","value":"852"},"status":"published"},"_oai":{"id":"oai:toyama.repo.nii.ac.jp:00000852","sets":["74:77:133:147"]},"author_link":["132057","132056"],"item_3_alternative_title_19":{"attribute_name":"その他（別言語等）のタイトル","attribute_value_mlt":[{"subitem_alternative_title":"Climate Variation of Japanese Islands and Effect of Atmosphere and Ocean"}]},"item_3_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2013-03-15","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"2","bibliographicPageEnd":"188","bibliographicPageStart":"173","bibliographicVolumeNumber":"7","bibliographic_titles":[{"bibliographic_title":"富山大学人間発達科学部紀要"}]}]},"item_3_description_4":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"The climate variation involves phenomena which occur spatially and temporally from macro to micro scale.\nEspecially, the one on the local scale is clear around the land surface. Therefore climate variation was analyzed mainly around the land surface, widely, synoptically, and locally. The climate variation in the Japanese Islands is affected by land and sea, and varies seasonally. Thus, seasonal variation around the land and sea surface was analyzed. The main results are as follows: 1) On the wide scale, the thermal state of the Eurasian Continent and the North Pacific changes to the contrary from winter to summer, and vice versa. Furthermore, the thermal state difference between the continent and the ocean is large in winter, but is small in summer. In addition, the phase of annual variation delays on the ocean. The climate variation is basically brought about by these, and it is influenced largely by the inter-annual shift of seasonal change. 2) On the meso-scale, the difference of the thermal state between the marginal sea,Yellow Sea, Sea of Japan, and Sea of Okhotsk, and the chains of islands and the peninsulas around the seas, becomes clear in spring and fall. Especially, from spring to early summer, the sea surface temperature of the marginal seas is remarkably cooler than the land surface temperature of surrounding areas. Therefore, meso-scale anticyclones are more likely to develop. In the warm current areas of the marginal seas, the difference of temperature between land and sea becomes remarkable in severe winter. And meso-scale cyclones develop. 3) On the local scale, the thermal states of the land and sea surfaces interchange between the night and the day. The difference of temperature between land and sea surfaces is small in hot summer, but it is large in severe winter. Therefore the reverse of thermal state between the night and the day is clear in hot summer, and the sea surface has a great influence on climate variation. On the other hand, the reverse is not clear in severe winter and the influence of the sea surface on climate variation is small.","subitem_description_type":"Abstract"},{"subitem_description":"本年（2012），また一昨年（2010）年は，夏季に全国各地で猛暑日の出現がとくに多かった。全国17地点の平均による夏季（6-8月）気温は，2010年は1898年以降で第 1位であった（田中昌太郎・牛田信吾・萱場亙起，2012）。熊谷や多治見のほか，全国各地で同様に高温が出現する。その地球規模から局地的な要因の解析によれば，さまざまなスケールの要因が複合して影響している。\nたとえば，富山平野南部の昇温には山越え気流の影響が考えられる（田上善夫，2010a）。また，富山をはじめ，広域に昇温が現れるとき，暖気が涵養され，移流となる場合がみられる（田上善夫，2010b）。さらに，異常高温は，日本海側やオホーツク海沿岸などに現れる傾向があり，かつ日中に現れることが多いが，高温の出現には地域的な類似性がある（田上善夫，2011）。さらに，日によって全国最高気温の出現地点が変わるように，特定の地点のみがとくに高温となるわけではない。このことに示されるように，広域的な出現要因が基本にあるが，こうしたスケールでの大気の内部変動，総観規模での気団の出現が深く影響している。\nまたこうした高温は，その出現前後の期間に比べた昇温としてみれば，暑夏のみならずどの季節にも出現する。むしろ夏季以外の季節では，顕著な昇温は地域的な差異が大きく，その出現過程は複雑である。従来の研究の場合，対象範囲が陸上に偏するか，あるいは広域の大気状態を対象にしているために，高層の状態が中心に解析されることが多かった。こうした気温にみられるような季節的に異なる大気状態の変動には，陸上のみならず，海上，また上層の状態が重要であるため，それらを含めての解析が必要となる。影響する現象のスケールとして，東アジアのようなおよそ2000kmのスケール，中部地方のようなおよそ200kmのスケール，富山平野のようなおよそ20kmのスケールに分けて考えることができ，それぞれについて解析を行う。","subitem_description_type":"Abstract"}]},"item_3_description_40":{"attribute_name":"資源タイプ(DSpace)","attribute_value_mlt":[{"subitem_description":"Article","subitem_description_type":"Other"}]},"item_3_description_6":{"attribute_name":"引用","attribute_value_mlt":[{"subitem_description":"富山大学人間発達科学部紀要, 7巻2号, Page 173-188","subitem_description_type":"Other"}]},"item_3_full_name_3":{"attribute_name":"著者別名","attribute_value_mlt":[{"nameIdentifiers":[{"nameIdentifier":"132057","nameIdentifierScheme":"WEKO"}],"names":[{"name":"TAGAMI, Yoshio"}]}]},"item_3_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.15099/00000846","subitem_identifier_reg_type":"JaLC"}]},"item_3_publisher_33":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"富山大学人間発達科学部"}]},"item_3_source_id_10":{"attribute_name":"書誌レコードID","attribute_value_mlt":[{"subitem_source_identifier":"AA12181167","subitem_source_identifier_type":"NCID"}]},"item_3_source_id_8":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"1881316X","subitem_source_identifier_type":"ISSN"}]},"item_3_version_type_16":{"attribute_name":"著者版フラグ","attribute_value_mlt":[{"subitem_version_resource":"http://purl.org/coar/version/c_970fb48d4fbd8a85","subitem_version_type":"VoR"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"田上, 善夫"}],"nameIdentifiers":[{}]}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2016-02-15"}],"displaytype":"detail","filename":"01-13_7-2_173-188_2013_ver2.pdf","filesize":[{"value":"9.0 MB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"01-13_7-2_173-188_2013_ver2.pdf","url":"https://toyama.repo.nii.ac.jp/record/852/files/01-13_7-2_173-188_2013_ver2.pdf"},"version_id":"ecd19e2b-1085-4bbd-b162-8378e5dbb467"}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"気候変動","subitem_subject_scheme":"Other"},{"subitem_subject":"季節","subitem_subject_scheme":"Other"},{"subitem_subject":"大気","subitem_subject_scheme":"Other"},{"subitem_subject":"海洋","subitem_subject_scheme":"Other"},{"subitem_subject":"Climate variation","subitem_subject_scheme":"Other"},{"subitem_subject":"Season","subitem_subject_scheme":"Other"},{"subitem_subject":"Ocean","subitem_subject_scheme":"Other"},{"subitem_subject":"Atmosphere","subitem_subject_scheme":"Other"}]},"item_language":{"attribute_name":"言語","attribute_value_mlt":[{"subitem_language":"jpn"}]},"item_resource_type":{"attribute_name":"資源タイプ","attribute_value_mlt":[{"resourcetype":"departmental bulletin paper","resourceuri":"http://purl.org/coar/resource_type/c_6501"}]},"item_title":"日本列島の気候変動と大気・海洋の影響","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"日本列島の気候変動と大気・海洋の影響"}]},"item_type_id":"3","owner":"3","path":["147"],"pubdate":{"attribute_name":"公開日","attribute_value":"2013-03-11"},"publish_date":"2013-03-11","publish_status":"0","recid":"852","relation_version_is_last":true,"title":["日本列島の気候変動と大気・海洋の影響"],"weko_creator_id":"3","weko_shared_id":-1},"updated":"2023-07-25T15:27:25.227066+00:00"}