{"created":"2023-06-20T14:52:25.485018+00:00","id":20565,"links":{},"metadata":{"_buckets":{"deposit":"e6873bbc-17f1-49fd-b651-dcc411e8adf5"},"_deposit":{"created_by":1,"id":"20565","owners":[1],"pid":{"revision_id":0,"type":"depid","value":"20565"},"status":"published"},"_oai":{"id":"oai:jaxa.repo.nii.ac.jp:00020565","sets":["1543:1778:1791","1887:1891"]},"author_link":["196249","196250","196252","196247","196248","196251"],"item_5_biblio_info_10":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2006-03","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"187","bibliographicPageStart":"184","bibliographic_titles":[{"bibliographic_title":"第38回月・惑星シンポジウム"},{"bibliographic_title":"Proceedings of the 38th ISAS Lunar and Planetary Symposium","bibliographic_titleLang":"en"}]}]},"item_5_description_17":{"attribute_name":"抄録（英）","attribute_value_mlt":[{"subitem_description":"The scattering greenhouse effect of CO2 ice cloud has been proposed as a mechanism to make the Martian climate warm enough to support flowing water under a faint young Sun. We construct a one-dimensional radiative model for the CO2-H2O atmosphere and analyze cloud stability on the basis of the numerical estimation of the ice condensation or evaporation rate in a cloud layer. Our numerical analysis suggests that a CO2 ice cloud layer is stabilized and the global mean surface temperature rises above melting point of H2O when the atmospheric pressure is larger than 1 bar and the column number density of cloud condensation nuclei is kept at nearby 10(exp 10) m(exp -2). A negative feedback mechanism between the particle size change and the radiative cooling may stabilize warm climate on early Mars.","subitem_description_type":"Other"}]},"item_5_description_32":{"attribute_name":"資料番号","attribute_value_mlt":[{"subitem_description":"資料番号: AA0063350050","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宇宙科学研究本部"}]},"item_5_publisher_9":{"attribute_name":"出版者（英）","attribute_value_mlt":[{"subitem_publisher":"Institute of Space and Astronautical Science, Japan Aerospace Exploration Agency (JAXA/ISAS)"}]},"item_5_text_6":{"attribute_name":"著者所属","attribute_value_mlt":[{"subitem_text_value":"北海道大学 大学院理学研究科"},{"subitem_text_value":"国立環境研究所"},{"subitem_text_value":"北海道大学 大学院理学研究科"}]},"item_5_text_7":{"attribute_name":"著者所属（英）","attribute_value_mlt":[{"subitem_text_language":"en","subitem_text_value":"Hokkaido University Graduate School of Science"},{"subitem_text_language":"en","subitem_text_value":"National Institute for Environmental Studies"},{"subitem_text_language":"en","subitem_text_value":"Hokkaido University Graduate School of Science"}]},"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":"光田, 千紘"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"横畠, 徳太"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"倉本, 圭"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Mitsuda, Chihiro","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Yokohata, Tokuta","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Kuramoto, Kiyoshi","creatorNameLang":"en"}],"nameIdentifiers":[{}]}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"惑星気象学","subitem_subject_scheme":"Other"},{"subitem_subject":"火星","subitem_subject_scheme":"Other"},{"subitem_subject":"惑星大気","subitem_subject_scheme":"Other"},{"subitem_subject":"火星大気","subitem_subject_scheme":"Other"},{"subitem_subject":"光散乱","subitem_subject_scheme":"Other"},{"subitem_subject":"温室効果","subitem_subject_scheme":"Other"},{"subitem_subject":"氷晶雲","subitem_subject_scheme":"Other"},{"subitem_subject":"気候安定性","subitem_subject_scheme":"Other"},{"subitem_subject":"2酸化炭素","subitem_subject_scheme":"Other"},{"subitem_subject":"水","subitem_subject_scheme":"Other"},{"subitem_subject":"凝縮核","subitem_subject_scheme":"Other"},{"subitem_subject":"放射伝達","subitem_subject_scheme":"Other"},{"subitem_subject":"planetary meteorology","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"Mars","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"planetary atmosphere","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"Martian atmosphere","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"light scattering","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"greenhouse effect","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"ice cloud","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"climate stability","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"carbon dioxide","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"water","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"condensation nucleus","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"radiative transfer","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":"conference paper","resourceuri":"http://purl.org/coar/resource_type/c_5794"}]},"item_title":"Scattering greenhouse effect of CO2 ice cloud and climate stability on early Mars","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"Scattering greenhouse effect of CO2 ice cloud and climate stability on early Mars","subitem_title_language":"en"}]},"item_type_id":"5","owner":"1","path":["1791","1891"],"pubdate":{"attribute_name":"公開日","attribute_value":"2015-03-26"},"publish_date":"2015-03-26","publish_status":"0","recid":"20565","relation_version_is_last":true,"title":["Scattering greenhouse effect of CO2 ice cloud and climate stability on early Mars"],"weko_creator_id":"1","weko_shared_id":-1},"updated":"2023-06-21T03:48:29.237021+00:00"}