{"created":"2023-04-20T01:18:42.327837+00:00","id":2000420,"links":{},"metadata":{"_buckets":{"deposit":"6742f469-617d-46a9-b81f-311349e20f12"},"_deposit":{"created_by":15,"id":"2000420","owner":"15","owners":[15],"owners_ext":{"displayname":"北見工業大学学術機関リポジトリ（KIT-R）","username":"kitir"},"pid":{"revision_id":0,"type":"depid","value":"2000420"},"status":"published"},"_oai":{"id":"oai:kitami-it.repo.nii.ac.jp:02000420","sets":["1:87"]},"author_link":[],"item_1646810750418":{"attribute_name":"出版タイプ","attribute_value_mlt":[{"subitem_version_resource":"http://purl.org/coar/version/c_970fb48d4fbd8a85","subitem_version_type":"VoR"}]},"item_3_biblio_info_186":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDateType":"Issued"},"bibliographicPageStart":"107845","bibliographicVolumeNumber":"273","bibliographic_titles":[{"bibliographic_title":"Journal of Quantitative Spectroscopy & Radiative Transfer","bibliographic_titleLang":"en"}]}]},"item_3_description_184":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"The properties of light reflected from snow and ice surfaces are important for the understanding of light\nscattering theory and the interpretation of remote sensing in the cryosphere. Spectral measurements\nof the degree of linear polarization (DoLP) and its related Stokes parameters Pq = −Q/I and Pu = U/I of\nStokes vector IS = [I Q U V]T were made for various snow and ice surfaces in Hokkaido, Japan. The measurement results indicated that the angular dependence on both the viewing angle and azimuth angle\nin the DoLP, Pq and Pu was significant especially in the shortwave infrared (SWIR) regions. In addition,\nan important finding here is that the measurements revealed for the first time the existence of neutral\npoints of Pq and Pu in the snow and bare ice surface. The SWIR polarization features can be explained by\nthe single scattering properties of snow/ice or surface reflection associated with surface scattering. For\nthe snow cases, the DoLP was represented by the measurement geometry and the scattering phase matrix while for the bare ice case, the DoLP was represented by the measurement geometry and the Fresnel\nreflection matrix. An additional remark is that the angular dependence of the neutral points was linked\nexclusively to the measurement geometry regardless of snow particle size, shape and scattering/absorbing\ninclusions in the ice. In contrast, the polarization in the visible regions was so small but remained detectable. However, the angular dependence of the neutral points was somewhat different from that in\nnear infrared and SWIR regions. These results suggested that the neutral points depend on the polarization magnitude and the plane of polarization that related to the multiple scattering in the snow and\natmosphere. The polarimetric measurements related to the neutral points are expected to be useful for\nthe retrieval of new snow/ice physical parameters","subitem_description_language":"en","subitem_description_type":"Abstract"}]},"item_3_publisher_212":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"Elsevier","subitem_publisher_language":"en"}]},"item_3_relation_191":{"attribute_name":"DOI","attribute_value_mlt":[{"subitem_relation_type_id":{"subitem_relation_type_id_text":"https://doi.org/10.1016/j.jqsrt.2021.107845","subitem_relation_type_select":"DOI"}}]},"item_3_rights_192":{"attribute_name":"権利","attribute_value_mlt":[{"subitem_rights":"© 2021 The Authors.","subitem_rights_language":"en"}]},"item_3_select_195":{"attribute_name":"著者版フラグ","attribute_value_mlt":[{"subitem_select_item":"publisher","subitem_select_language":"en"}]},"item_access_right":{"attribute_name":"アクセス権","attribute_value_mlt":[{"subitem_access_right":"open access","subitem_access_right_uri":"http://purl.org/coar/access_right/c_abf2"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"Tomonori Tanikawa","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"Kazuhiko Masuda","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"Hiroshi Ishimoto","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"Teruo Aoki","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"Masahiro Hori","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"Masashi Niwano","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"Akihiro Hachikubo","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"Sumito Matoba","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"Konosuke Sugiura","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"Takenobu Toyota","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"Nozomu Ohkawara","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"Knut Stamnes","creatorNameLang":"en"}]}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_access","date":[{"dateType":"Available","dateValue":"2023-04-20"}],"filename":"1-s2.0-S0022407321003381-main.pdf","filesize":[{"value":"6.4 MB"}],"format":"application/pdf","licensetype":"license_0","url":{"url":"https://kitami-it.repo.nii.ac.jp/record/2000420/files/1-s2.0-S0022407321003381-main.pdf"},"version_id":"8049f59b-860e-4cba-8b2f-da7a4200b7b2"}]},"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":"journal article","resourceuri":"http://purl.org/coar/resource_type/c_6501"}]},"item_title":"Spectral degree of linear polarization and neutral points of polarization in snow and ice surfaces","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"Spectral degree of linear polarization and neutral points of polarization in snow and ice surfaces","subitem_title_language":"en"}]},"item_type_id":"3","owner":"15","path":["87"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2023-04-20"},"publish_date":"2023-04-20","publish_status":"0","recid":"2000420","relation_version_is_last":true,"title":["Spectral degree of linear polarization and neutral points of polarization in snow and ice surfaces"],"weko_creator_id":"15","weko_shared_id":-1},"updated":"2023-04-20T01:30:17.837827+00:00"}