ログイン サインアップ
言語:

WEKO3

  • トップ
  • ランキング
To
lat lon distance
To

Field does not validate



インデックスリンク

インデックスツリー

メールアドレスを入力してください。

WEKO

One fine body…

WEKO

One fine body…

アイテム

{"_buckets": {"deposit": "46ebd402-0e3d-475c-92d8-3f32ee15b1e7"}, "_deposit": {"id": "5925", "owners": [1], "pid": {"revision_id": 0, "type": "depid", "value": "5925"}, "status": "published"}, "_oai": {"id": "oai:nied-repo.bosai.go.jp:00005925", "sets": []}, "author_link": [], "item_10001_biblio_info_7": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "2014", "bibliographicIssueDateType": "Issued"}, "bibliographicIssueNumber": "0", "bibliographicPageEnd": "53", "bibliographicPageStart": "47", "bibliographicVolumeNumber": "32", "bibliographic_titles": [{"bibliographic_title": "BULLETIN OF GLACIOLOGICAL RESEARCH", "bibliographic_titleLang": "en"}]}]}, "item_10001_description_5": {"attribute_name": "抄録", "attribute_value_mlt": [{"subitem_description": "The specific surface area (SSA) of snow is of particular interest to researchers because SSA is strongly related to snow albedo and is a comparatively better indicator of snow\u0027s complexity than grain size. The time variation of SSA for fresh snow samples was observed in the laboratory under isothermal conditions at 226 K and 254 K using the gas adsorption method and Brunauer-Emmett-Teller theory. The SSA of the snow samples decreased with time under isothermal metamorphism. The decrease in SSA was fitted with the logarithmic equation proposed by Legagneux et al. (2003), and adjustable parameters were obtained. The rate of decrease in SSA depended on the shape of the initial snow type and temperature. Dendritic snow samples exhibited large initial SSAs, and their SSAs decreased faster compared with those of fragmented (collected from drifting snow) and plate-like precipitation particles with relatively small initial SSAs. The rate of decrease in SSA was lower at 226 K than that at 254 K.", "subitem_description_language": "en", "subitem_description_type": "Other"}]}, "item_10001_publisher_8": {"attribute_name": "出版者", "attribute_value_mlt": [{"subitem_publisher": "NIHON SEPPYO GAKKAI-JAPANESE SOC SNOW \u0026 ICE", "subitem_publisher_language": "en"}]}, "item_10001_relation_14": {"attribute_name": "DOI", "attribute_value_mlt": [{"subitem_relation_type_id": {"subitem_relation_type_id_text": "10.5331/bgr.32.47"}}]}, "item_10001_source_id_9": {"attribute_name": "ISSN", "attribute_value_mlt": [{"subitem_source_identifier": "1884-8044", "subitem_source_identifier_type": "EISSN"}]}, "item_creator": {"attribute_name": "著者", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "Akihiro Hachikubo", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Satoru Yamaguchi", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Hayato Arakawa", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Tomonori Tanikawa", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Masahiro Hori", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Konosuke Sugiura", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Sumito Matoba", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Masashi Niwano", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Katsuyuki Kuchiki", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Teruo Aoki", "creatorNameLang": "en"}]}]}, "item_language": {"attribute_name": "言語", "attribute_value_mlt": [{"subitem_language": "eng"}]}, "item_title": "Effects of temperature and grain type on time variation of snow specific surface area", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "Effects of temperature and grain type on time variation of snow specific surface area", "subitem_title_language": "en"}]}, "item_type_id": "40001", "owner": "1", "path": ["1670839190650"], "permalink_uri": "https://nied-repo.bosai.go.jp/records/5925", "pubdate": {"attribute_name": "PubDate", "attribute_value": "2023-03-30"}, "publish_date": "2023-03-30", "publish_status": "0", "recid": "5925", "relation": {}, "relation_version_is_last": true, "title": ["Effects of temperature and grain type on time variation of snow specific surface area"], "weko_shared_id": -1}
  1. 防災科研関係論文

Effects of temperature and grain type on time variation of snow specific surface area

https://nied-repo.bosai.go.jp/records/5925
https://nied-repo.bosai.go.jp/records/5925
1250fbd4-6d2e-4786-a686-453f70430be5
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 en
タイトル Effects of temperature and grain type on time variation of snow specific surface area
言語
言語 eng
著者 Akihiro Hachikubo

× Akihiro Hachikubo

en Akihiro Hachikubo

Search repository
Satoru Yamaguchi

× Satoru Yamaguchi

en Satoru Yamaguchi

Search repository
Hayato Arakawa

× Hayato Arakawa

en Hayato Arakawa

Search repository
Tomonori Tanikawa

× Tomonori Tanikawa

en Tomonori Tanikawa

Search repository
Masahiro Hori

× Masahiro Hori

en Masahiro Hori

Search repository
Konosuke Sugiura

× Konosuke Sugiura

en Konosuke Sugiura

Search repository
Sumito Matoba

× Sumito Matoba

en Sumito Matoba

Search repository
Masashi Niwano

× Masashi Niwano

en Masashi Niwano

Search repository
Katsuyuki Kuchiki

× Katsuyuki Kuchiki

en Katsuyuki Kuchiki

Search repository
Teruo Aoki

× Teruo Aoki

en Teruo Aoki

Search repository
抄録
内容記述タイプ Other
内容記述 The specific surface area (SSA) of snow is of particular interest to researchers because SSA is strongly related to snow albedo and is a comparatively better indicator of snow's complexity than grain size. The time variation of SSA for fresh snow samples was observed in the laboratory under isothermal conditions at 226 K and 254 K using the gas adsorption method and Brunauer-Emmett-Teller theory. The SSA of the snow samples decreased with time under isothermal metamorphism. The decrease in SSA was fitted with the logarithmic equation proposed by Legagneux et al. (2003), and adjustable parameters were obtained. The rate of decrease in SSA depended on the shape of the initial snow type and temperature. Dendritic snow samples exhibited large initial SSAs, and their SSAs decreased faster compared with those of fragmented (collected from drifting snow) and plate-like precipitation particles with relatively small initial SSAs. The rate of decrease in SSA was lower at 226 K than that at 254 K.
言語 en
書誌情報 en : BULLETIN OF GLACIOLOGICAL RESEARCH

巻 32, 号 0, p. 47-53, 発行日 2014
出版者
言語 en
出版者 NIHON SEPPYO GAKKAI-JAPANESE SOC SNOW & ICE
ISSN
収録物識別子タイプ EISSN
収録物識別子 1884-8044
DOI
関連識別子 10.5331/bgr.32.47
戻る
0
views
See details
Views

Versions

Ver.1 2023-03-31 02:46:49.488740
Show All versions

エクスポート

OAI-PMH
  • OAI-PMH JPCOAR
  • OAI-PMH DublinCore
  • OAI-PMH DDI
Other Formats
  • JSON
  • BIBTEX

Confirm


Powered by WEKO3

Change consent settings


Powered by WEKO3

Change consent settings