{"created":"2023-03-31T02:09:05.036092+00:00","id":4966,"links":{},"metadata":{"_buckets":{"deposit":"d69870ee-9291-4082-b611-b852add4aad9"},"_deposit":{"id":"4966","owners":[1],"pid":{"revision_id":0,"type":"depid","value":"4966"},"status":"published"},"_oai":{"id":"oai:nied-repo.bosai.go.jp:00004966","sets":[]},"author_link":[],"item_10001_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2014-10","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"10","bibliographicPageEnd":"2245","bibliographicPageStart":"2232","bibliographicVolumeNumber":"53","bibliographic_titles":[{"bibliographic_title":"JOURNAL OF APPLIED METEOROLOGY AND CLIMATOLOGY","bibliographic_titleLang":"en"}]}]},"item_10001_description_5":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"The liquid water fraction of individual snowflakes f is an important parameter when calculating the radar reflectivity of a melting layer. A ground-based observation of fat Nagaoka, Japan, was conducted by using dye-treated filter papers that were kept at a temperature of 0 degrees C. From the results of these measurements, which consisted of 6179 particles taken with 44 sheets of filter paper, two empirical relationships are proposed. The first is a relationship between the ratio of liquid water flux to total precipitation intensity (F-L; taking values from 0 to 1) and meteorological surface data. The second is a relationship to estimate fusing the melted diameter of a snowflake, median mass diameter, and F-L. It was determined that the root-mean-square errors for estimating F-L and f by using these relationships were 0.160 and 0.144, respectively. It was also found that the ratio of raindrop flux to the total precipitation intensity F-R was always below 0.1 when F-L was less than 0.6 but increased rapidly when F-L exceeded 0.8.","subitem_description_language":"en","subitem_description_type":"Other"}]},"item_10001_publisher_8":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"AMER METEOROLOGICAL SOC","subitem_publisher_language":"en"}]},"item_10001_relation_14":{"attribute_name":"DOI","attribute_value_mlt":[{"subitem_relation_type_id":{"subitem_relation_type_id_text":"10.1175/JAMC-D-13-0169.1"}}]},"item_10001_source_id_9":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"1558-8432","subitem_source_identifier_type":"EISSN"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"Ryohei Misumi","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"Hiroki Motoyoshi","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"Satoru Yamaguchi","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"Sento Nakai","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"Masaaki Ishizaka","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"Yasushi Fujiyoshi","creatorNameLang":"en"}]}]},"item_language":{"attribute_name":"言語","attribute_value_mlt":[{"subitem_language":"eng"}]},"item_title":"Empirical Relationships for Estimating Liquid Water Fraction of Melting Snowflakes","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"Empirical Relationships for Estimating Liquid Water Fraction of Melting Snowflakes","subitem_title_language":"en"}]},"item_type_id":"40001","owner":"1","path":["1670839190650"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2023-03-30"},"publish_date":"2023-03-30","publish_status":"0","recid":"4966","relation_version_is_last":true,"title":["Empirical Relationships for Estimating Liquid Water Fraction of Melting Snowflakes"],"weko_creator_id":"1","weko_shared_id":-1},"updated":"2023-06-08T06:13:31.382146+00:00"}