{"created":"2023-06-20T14:39:15.461099+00:00","id":5973,"links":{},"metadata":{"_buckets":{"deposit":"bf9c3b19-0eb4-4de3-8484-95ece3cd05b5"},"_deposit":{"created_by":1,"id":"5973","owners":[1],"pid":{"revision_id":0,"type":"depid","value":"5973"},"status":"published"},"_oai":{"id":"oai:jaxa.repo.nii.ac.jp:00005973","sets":["1887:1891","9:789:998:1024"]},"author_link":["29615","29616","29614","29613"],"item_5_alternative_title_2":{"attribute_name":"その他のタイトル（英）","attribute_value_mlt":[{"subitem_alternative_title":"High-resolution numerical prediction for aviation weather"}]},"item_5_biblio_info_10":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2006-12-01","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"162","bibliographicPageStart":"157","bibliographicVolumeNumber":"JAXA-SP-06-010","bibliographic_titles":[{"bibliographic_title":"宇宙航空研究開発機構特別資料: 航空宇宙数値シミュレーション技術シンポジウム2006論文集"},{"bibliographic_title":"JAXA Special Publication: Proceedings of Aerospace Numerical Simulation Symposium 2006","bibliographic_titleLang":"en"}]}]},"item_5_description_17":{"attribute_name":"抄録（英）","attribute_value_mlt":[{"subitem_description":"The Japan Meteorological Agency (JMA) operates a suite of numerical weather prediction models; the Meso-Scale Model (MSM), the Regional Spectral Model (RSM), and the Global Spectral Model (GSM) with horizontal grid spacing of 5 km, 20 km and 60 km respectively. In addition, a high-resolution Local Forecast Mode (LFM) with grid spacing of 2 km has been developed so as to prevent disaster and maintain safe civil aviation at JMA. With this model, numerical experiments of a wind shear in Haneda Airport on February 26, 2006 associated with a Cold Front Aloft (CFA) and dry trough were carried out on the supercomputer of CeNSS. The LFM successfully reproduced the observed time series variation of the wind at Haneda Airport, although the MSM failed to predict the ending time of the southerly wind. The reason is that the dry trough interacted with CFA did not propagate correctly in the MSM. The analysis using the frontogenetical function reveals that the frontolysis led by the one vertical circulation near the nose of CFA took place and resulted to the prevention of intensification of the front. On the other hand, the LFM could simulate the several vertical circulations so that the frontogenesis and the frontolysis appeared at different circulations. These results suggest the frontogenesis (frontolysis) is occurring more appropriately at finer resolution.","subitem_description_type":"Other"}]},"item_5_description_32":{"attribute_name":"資料番号","attribute_value_mlt":[{"subitem_description":"資料番号: AA0063154029","subitem_description_type":"Other"}]},"item_5_description_33":{"attribute_name":"レポート番号","attribute_value_mlt":[{"subitem_description":"レポート番号: JAXA-SP-06-010","subitem_description_type":"Other"}]},"item_5_publisher_8":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"宇宙航空研究開発機構"}]},"item_5_publisher_9":{"attribute_name":"出版者（英）","attribute_value_mlt":[{"subitem_publisher":"Japan Aerospace Exploration Agency (JAXA)"}]},"item_5_source_id_21":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"1349-113X","subitem_source_identifier_type":"ISSN"}]},"item_5_source_id_24":{"attribute_name":"書誌レコードID","attribute_value_mlt":[{"subitem_source_identifier":"AA11984031","subitem_source_identifier_type":"NCID"}]},"item_5_text_6":{"attribute_name":"著者所属","attribute_value_mlt":[{"subitem_text_value":"気象庁"},{"subitem_text_value":"気象庁"}]},"item_5_text_7":{"attribute_name":"著者所属（英）","attribute_value_mlt":[{"subitem_text_language":"en","subitem_text_value":"Japan Meteorological Agency"},{"subitem_text_language":"en","subitem_text_value":"Japan Meteorological Agency"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"中山, 寛"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"本田, 有機"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Nakayama, Hiroshi","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Honda, Yuki","creatorNameLang":"en"}],"nameIdentifiers":[{}]}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2020-01-16"}],"displaytype":"detail","filename":"63154029.pdf","filesize":[{"value":"2.2 MB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"63154029.pdf","url":"https://jaxa.repo.nii.ac.jp/record/5973/files/63154029.pdf"},"version_id":"758cc238-f511-4132-a4c2-8ce76fe1d128"}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"数値天気予報","subitem_subject_scheme":"Other"},{"subitem_subject":"航空気象","subitem_subject_scheme":"Other"},{"subitem_subject":"メソモデル","subitem_subject_scheme":"Other"},{"subitem_subject":"領域モデル","subitem_subject_scheme":"Other"},{"subitem_subject":"全球モデル","subitem_subject_scheme":"Other"},{"subitem_subject":"寒冷前線","subitem_subject_scheme":"Other"},{"subitem_subject":"風向","subitem_subject_scheme":"Other"},{"subitem_subject":"雨","subitem_subject_scheme":"Other"},{"subitem_subject":"気温","subitem_subject_scheme":"Other"},{"subitem_subject":"運行業務","subitem_subject_scheme":"Other"},{"subitem_subject":"精度","subitem_subject_scheme":"Other"},{"subitem_subject":"前線発達","subitem_subject_scheme":"Other"},{"subitem_subject":"前線消滅","subitem_subject_scheme":"Other"},{"subitem_subject":"numerical weather forecasting","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"aviation meteorology","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"meso-scale model","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"regional scale model","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"global scale model","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"cold front","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"wind direction","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"rain","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"atmospheric temperature","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"flight operation","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"accuracy","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"frontogenesis","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"frontolysis","subitem_subject_language":"en","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":"conference paper","resourceuri":"http://purl.org/coar/resource_type/c_5794"}]},"item_title":"航空機の運航に影響を与える気象の高解像度数値予報","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"航空機の運航に影響を与える気象の高解像度数値予報"}]},"item_type_id":"5","owner":"1","path":["1024","1891"],"pubdate":{"attribute_name":"公開日","attribute_value":"2015-03-26"},"publish_date":"2015-03-26","publish_status":"0","recid":"5973","relation_version_is_last":true,"title":["航空機の運航に影響を与える気象の高解像度数値予報"],"weko_creator_id":"1","weko_shared_id":-1},"updated":"2023-06-21T08:05:00.458381+00:00"}