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": "378cce35-5694-4c63-a5fb-457e062b844c"}, "_deposit": {"id": "5560", "owners": [1], "pid": {"revision_id": 0, "type": "depid", "value": "5560"}, "status": "published"}, "_oai": {"id": "oai:nied-repo.bosai.go.jp:00005560", "sets": []}, "author_link": [], "item_10001_biblio_info_7": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "2016-06", "bibliographicIssueDateType": "Issued"}, "bibliographicPageEnd": "145", "bibliographicPageStart": "140", "bibliographicVolumeNumber": "12", "bibliographic_titles": [{"bibliographic_title": "SOLA (Scientific Online Letters on the Atmosphere)", "bibliographic_titleLang": "ja"}, {"bibliographic_title": "SOLA (Scientific Online Letters on the Atmosphere)", "bibliographic_titleLang": "en"}]}]}, "item_10001_description_5": {"attribute_name": "抄録", "attribute_value_mlt": [{"subitem_description": "Supercooled liquid droplets (SLDs) not only play important roles in precipitation formation processes but they also affect the radiation budget. Therefore, it is important to clarify the distribution and quantity of SLDs. Hydrometeor videosonde observations were performed in February 2011 at Rikubetsu in inland Hokkaido, Japan. Five hydrometeor videosondes were released in ice precipitations in stratiform clouds and SLDs were detected in three cases. The clouds in these three cases had SLDs at the cloud tops. The microphysical quantities of the SLD layers were within the ranges of those observed in Arctic mixed-phase clouds. The cloud-top SLDs had potential to cause radiative cooling, which contributed to the formation of upward motion generating ice precipitation. Small water vapor amounts above the cloud tops cannot contribute to moisture supply. Vertical profiles of temperature and moisture showed that the SLD layers were decoupled from surface moisture sources. The absence of additional moisture supply was consistent with short lifetimes, compared with persistent Arctic mixed-phase clouds.", "subitem_description_language": "en", "subitem_description_type": "Other"}]}, "item_10001_publisher_8": {"attribute_name": "出版者", "attribute_value_mlt": [{"subitem_publisher": "METEOROLOGICAL SOC JAPAN", "subitem_publisher_language": "en"}]}, "item_10001_relation_14": {"attribute_name": "DOI", "attribute_value_mlt": [{"subitem_relation_type_id": {"subitem_relation_type_id_text": "10.2151/sola.2016-030"}}]}, "item_10001_source_id_9": {"attribute_name": "ISSN", "attribute_value_mlt": [{"subitem_source_identifier": "1349-6476", "subitem_source_identifier_type": "ISSN"}]}, "item_creator": {"attribute_name": "著者", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "Tadayasu Ohigashi", "creatorNameLang": "ja"}, {"creatorName": "Tadayasu Ohigashi", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Kazuhisa Tsuboki", "creatorNameLang": "ja"}, {"creatorName": "Kazuhisa Tsuboki", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Mariko Oue", "creatorNameLang": "ja"}, {"creatorName": "Mariko Oue", "creatorNameLang": "en"}]}]}, "item_language": {"attribute_name": "言語", "attribute_value_mlt": [{"subitem_language": "eng"}]}, "item_title": "Cloud-top supercooled liquid droplets in stratiform clouds observed during winter in inland Hokkaido, Japan", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "Cloud-top supercooled liquid droplets in stratiform clouds observed during winter in inland Hokkaido, Japan", "subitem_title_language": "ja"}, {"subitem_title": "Cloud-top supercooled liquid droplets in stratiform clouds observed during winter in inland Hokkaido, Japan", "subitem_title_language": "en"}]}, "item_type_id": "40001", "owner": "1", "path": ["1670839190650"], "permalink_uri": "https://nied-repo.bosai.go.jp/records/5560", "pubdate": {"attribute_name": "PubDate", "attribute_value": "2023-07-10"}, "publish_date": "2023-07-10", "publish_status": "0", "recid": "5560", "relation": {}, "relation_version_is_last": true, "title": ["Cloud-top supercooled liquid droplets in stratiform clouds observed during winter in inland Hokkaido, Japan"], "weko_shared_id": -1}
  1. 防災科研関係論文

Cloud-top supercooled liquid droplets in stratiform clouds observed during winter in inland Hokkaido, Japan

https://nied-repo.bosai.go.jp/records/5560
https://nied-repo.bosai.go.jp/records/5560
fa127d1a-b891-4e2f-ae00-ace48e583fd9
Item type researchmap(1)
公開日 2023-07-10
タイトル
言語 ja
タイトル Cloud-top supercooled liquid droplets in stratiform clouds observed during winter in inland Hokkaido, Japan
タイトル
言語 en
タイトル Cloud-top supercooled liquid droplets in stratiform clouds observed during winter in inland Hokkaido, Japan
言語
言語 eng
著者 Tadayasu Ohigashi

× Tadayasu Ohigashi

ja Tadayasu Ohigashi

en Tadayasu Ohigashi

Search repository
Kazuhisa Tsuboki

× Kazuhisa Tsuboki

ja Kazuhisa Tsuboki

en Kazuhisa Tsuboki

Search repository
Mariko Oue

× Mariko Oue

ja Mariko Oue

en Mariko Oue

Search repository
抄録
内容記述タイプ Other
内容記述 Supercooled liquid droplets (SLDs) not only play important roles in precipitation formation processes but they also affect the radiation budget. Therefore, it is important to clarify the distribution and quantity of SLDs. Hydrometeor videosonde observations were performed in February 2011 at Rikubetsu in inland Hokkaido, Japan. Five hydrometeor videosondes were released in ice precipitations in stratiform clouds and SLDs were detected in three cases. The clouds in these three cases had SLDs at the cloud tops. The microphysical quantities of the SLD layers were within the ranges of those observed in Arctic mixed-phase clouds. The cloud-top SLDs had potential to cause radiative cooling, which contributed to the formation of upward motion generating ice precipitation. Small water vapor amounts above the cloud tops cannot contribute to moisture supply. Vertical profiles of temperature and moisture showed that the SLD layers were decoupled from surface moisture sources. The absence of additional moisture supply was consistent with short lifetimes, compared with persistent Arctic mixed-phase clouds.
言語 en
書誌情報 ja : SOLA (Scientific Online Letters on the Atmosphere)
en : SOLA (Scientific Online Letters on the Atmosphere)

巻 12, p. 140-145, 発行日 2016-06
出版者
言語 en
出版者 METEOROLOGICAL SOC JAPAN
ISSN
収録物識別子タイプ ISSN
収録物識別子 1349-6476
DOI
関連識別子 10.2151/sola.2016-030
戻る
0
views
See details
Views

Versions

Ver.1 2023-03-31 02:34:55.613757
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