{"created":"2023-05-15T16:35:06.328025+00:00","id":7966,"links":{},"metadata":{"_buckets":{"deposit":"5b10956d-b8ae-4705-8538-552b896378da"},"_deposit":{"created_by":2,"id":"7966","owners":[2],"pid":{"revision_id":0,"type":"depid","value":"7966"},"status":"published"},"_oai":{"id":"oai:nagasaki-u.repo.nii.ac.jp:00007966","sets":["52:572"]},"author_link":["32829","32828"],"item_9_biblio_info_6":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2013","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"427","bibliographicPageStart":"424","bibliographicVolumeNumber":"1531","bibliographic_titles":[{"bibliographic_title":"AIP Conference Proceedings"}]}]},"item_9_description_4":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"The relationship between the precipitation stage and water cloud properties was studied in the mid-latitudes using space-borne radar and radiometer data, with a focus on a comparison between continental (over China) and oceanic (over the northwest Pacific) clouds. More specifically, fractional occurrences of the precipitation categories were investigated in terms of two-dimensional representations of cloud parameters, such as combinations of optical depth - effective particle radius, and liquid water path - droplet number density. As a result, systematic changes in the transition regarding pairs of the cloud parameters were well captured for all precipitation categories. The transition pattern was similar for both land and oceanic clouds. Notably, the ranges of all values of cloud parameters (except cloud droplet number density) were considerably larger for oceanic clouds for the precipitating category.","subitem_description_type":"Abstract"}]},"item_9_description_5":{"attribute_name":"内容記述","attribute_value_mlt":[{"subitem_description":"International Radiation Symposium: Radiation Processes in the Atmosphere and Ocean, IRS 2012; Berlin; Germany; 6 August 2012 ～ 10 August 2012","subitem_description_type":"Other"}]},"item_9_description_63":{"attribute_name":"引用","attribute_value_mlt":[{"subitem_description":"AIP Conference Proceedings, 1531, pp.424-427; 2013","subitem_description_type":"Other"}]},"item_9_publisher_33":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"American Institute of Physics Inc."}]},"item_9_relation_12":{"attribute_name":"DOI","attribute_value_mlt":[{"subitem_relation_type":"isIdenticalTo","subitem_relation_type_id":{"subitem_relation_type_id_text":"10.1063/1.4804797","subitem_relation_type_select":"DOI"}}]},"item_9_rights_13":{"attribute_name":"権利","attribute_value_mlt":[{"subitem_rights":"© 2013 American Institute of Physics. This article may be downloaded for personal use only. Any other use requires prior permission of the author and the American Institute of Physics. The following article appeared in AIP Conference Proceedings, 1531, pp.424-427; 2013 and may be found at http://dx.doi.org/10.1063/1.4804797"}]},"item_9_source_id_7":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"0094243X","subitem_source_identifier_type":"ISSN"}]},"item_9_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":"Kawamoto, Kazuaki"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Suzuki, Kentaroh"}],"nameIdentifiers":[{}]}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2020-12-21"}],"displaytype":"detail","filename":"AIPCP1531_424.pdf","filesize":[{"value":"746.9 kB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"AIPCP1531_424.pdf","url":"https://nagasaki-u.repo.nii.ac.jp/record/7966/files/AIPCP1531_424.pdf"},"version_id":"40b09bd5-5541-437c-a001-f510449cf652"}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"Clouds","subitem_subject_scheme":"Other"},{"subitem_subject":"Drizzle","subitem_subject_scheme":"Other"},{"subitem_subject":"Microphysical properties","subitem_subject_scheme":"Other"},{"subitem_subject":"Precipitation","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":"conference paper","resourceuri":"http://purl.org/coar/resource_type/c_5794"}]},"item_title":"Difference in fractional occurrences of precipitation categories in terms of cloud properties","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"Difference in fractional occurrences of precipitation categories in terms of cloud properties"}]},"item_type_id":"9","owner":"2","path":["572"],"pubdate":{"attribute_name":"公開日","attribute_value":"2013-07-18"},"publish_date":"2013-07-18","publish_status":"0","recid":"7966","relation_version_is_last":true,"title":["Difference in fractional occurrences of precipitation categories in terms of cloud properties"],"weko_creator_id":"2","weko_shared_id":-1},"updated":"2023-05-16T02:14:59.422163+00:00"}