ログイン
言語:

WEKO3

  • トップ
  • コミュニティ
  • ランキング
AND
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": "5603318e-7fe5-44eb-9e18-40d7971d68cc"}, "_deposit": {"id": "9565", "owners": [], "pid": {"revision_id": 0, "type": "depid", "value": "9565"}, "status": "published"}, "_oai": {"id": "oai:nagoya.repo.nii.ac.jp:00009565"}, "item_10_biblio_info_6": {"attribute_name": "\u66f8\u8a8c\u60c5\u5831", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "2007", "bibliographicIssueDateType": "Issued"}, "bibliographicPageEnd": "2891", "bibliographicPageStart": "2882", "bibliographicVolumeNumber": "21", "bibliographic_titles": [{"bibliographic_title": "HYDROLOGICAL PROCESSES"}]}]}, "item_10_description_4": {"attribute_name": "\u6284\u9332", "attribute_value_mlt": [{"subitem_description": "Model calculations are made in order to understand the characteristics and response to climate change of runoff from a cold glacier on the Tibetan Plateau. Some 20% of meltwater is preserved at the snow.ice boundary due to refreezing, since the glaciers in mid to northern Tibet are sufficiently cooled during the previous winter. Sensitivity to alterations in meteorological parameters has revealed that a change in air temperature would cause not only an increase in melting by sensible heat, but also a drastic increase in melting due to lowering of the albedo, since some of the snowfall changes to rainfall. In addition, it was suggested that a decrease in precipitation would cause a lowering of the surface albedo, with a resulting increase in the contribution of glacier runoff to the total runoff of river water. This study shows the first quantitative evaluation of the above effects, though they have been suggested qualitatively. The seasonal sensitivity of glacier runoff was examined by changing the dates given for a meteorological perturbation for a period of only 5 days. It was revealed that changes in both air temperature and precipitation during the melting season strongly affected glacier runoff by changing the surface albedo, though these perturbations only slightly altered the annual averages.", "subitem_description_type": "Abstract"}]}, "item_10_identifier_60": {"attribute_name": "URI", "attribute_value_mlt": [{"subitem_identifier_type": "HDL", "subitem_identifier_uri": "http://hdl.handle.net/2237/11361"}]}, "item_10_publisher_32": {"attribute_name": "\u51fa\u7248\u8005", "attribute_value_mlt": [{"subitem_publisher": "Wiley"}]}, "item_10_rights_12": {"attribute_name": "\u6a29\u5229", "attribute_value_mlt": [{"subitem_rights": "This is a preprint of an article published in HYDROLOGICAL PROCESSES. v.21, 2008, p.2882-2891http://www.interscience.wiley.com/"}]}, "item_10_select_15": {"attribute_name": "\u8457\u8005\u7248\u30d5\u30e9\u30b0", "attribute_value_mlt": [{"subitem_select_item": "author"}]}, "item_10_source_id_7": {"attribute_name": "ISSN", "attribute_value_mlt": [{"subitem_source_identifier": "08856087", "subitem_source_identifier_type": "ISSN"}]}, "item_10_text_14": {"attribute_name": "\u30d5\u30a9\u30fc\u30de\u30c3\u30c8", "attribute_value_mlt": [{"subitem_text_value": "application/pdf"}]}, "item_creator": {"attribute_name": "\u8457\u8005", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "Fujita, Koji"}], "nameIdentifiers": [{"nameIdentifier": "29110", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "\u85e4\u7530, \u8015\u53f2"}], "nameIdentifiers": [{"nameIdentifier": "29111", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "Ohta, Takeshi"}], "nameIdentifiers": [{"nameIdentifier": "29112", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "Ageta, Yutaka"}], "nameIdentifiers": [{"nameIdentifier": "29113", "nameIdentifierScheme": "WEKO"}]}]}, "item_files": {"attribute_name": "\u30d5\u30a1\u30a4\u30eb\u60c5\u5831", "attribute_type": "file", "attribute_value_mlt": [{"accessrole": "open_date", "date": [{"dateType": "Available", "dateValue": "2018-02-20"}], "displaytype": "detail", "download_preview_message": "", "file_order": 0, "filename": "2007HP21_fujita_a.pdf", "filesize": [{"value": "898.4 kB"}], "format": "application/pdf", "future_date_message": "", "is_thumbnail": false, "licensetype": "license_free", "mimetype": "application/pdf", "size": 898400.0, "url": {"label": "2007HP21_fujita_a.pdf", "url": "https://nagoya.repo.nii.ac.jp/record/9565/files/2007HP21_fujita_a.pdf"}, "version_id": "d161a02d-f653-44cf-8cca-65afbe8b7831"}]}, "item_keyword": {"attribute_name": "\u30ad\u30fc\u30ef\u30fc\u30c9", "attribute_value_mlt": [{"subitem_subject": "glacier", "subitem_subject_scheme": "Other"}, {"subitem_subject": "runoff", "subitem_subject_scheme": "Other"}, {"subitem_subject": "model", "subitem_subject_scheme": "Other"}, {"subitem_subject": "Tibet", "subitem_subject_scheme": "Other"}, {"subitem_subject": "climatic sensitivity", "subitem_subject_scheme": "Other"}, {"subitem_subject": "albedo", "subitem_subject_scheme": "Other"}]}, "item_language": {"attribute_name": "\u8a00\u8a9e", "attribute_value_mlt": [{"subitem_language": "eng"}]}, "item_resource_type": {"attribute_name": "\u8cc7\u6e90\u30bf\u30a4\u30d7", "attribute_value_mlt": [{"resourcetype": "journal article", "resourceuri": "http://purl.org/coar/resource_type/c_6501"}]}, "item_title": "Characteristics and climatic sensitivities of runoff from a cold-type glacier on the Tibetan Plateau", "item_titles": {"attribute_name": "\u30bf\u30a4\u30c8\u30eb", "attribute_value_mlt": [{"subitem_title": "Characteristics and climatic sensitivities of runoff from a cold-type glacier on the Tibetan Plateau"}]}, "item_type_id": "10", "owner": "1", "path": ["488/489/490"], "permalink_uri": "http://hdl.handle.net/2237/11361", "pubdate": {"attribute_name": "\u516c\u958b\u65e5", "attribute_value": "2009-03-27"}, "publish_date": "2009-03-27", "publish_status": "0", "recid": "9565", "relation": {}, "relation_version_is_last": true, "title": ["Characteristics and climatic sensitivities of runoff from a cold-type glacier on the Tibetan Plateau"], "weko_shared_id": 3}
  1. D300 大学院環境学研究科
  2. D300a 雑誌掲載論文
  3. 学術雑誌

Characteristics and climatic sensitivities of runoff from a cold-type glacier on the Tibetan Plateau

http://hdl.handle.net/2237/11361
3f764211-56e9-4b5d-8aa3-d550aed9c04a
名前 / ファイル ライセンス アクション
2007HP21_fujita_a.pdf 2007HP21_fujita_a.pdf (898.4 kB)
Item type 学術雑誌論文 / Journal Article(1)
公開日 2009-03-27
タイトル
タイトル Characteristics and climatic sensitivities of runoff from a cold-type glacier on the Tibetan Plateau
著者 Fujita, Koji

× Fujita, Koji

WEKO 29110

Fujita, Koji

Search repository
藤田, 耕史

× 藤田, 耕史

WEKO 29111

藤田, 耕史

Search repository
Ohta, Takeshi

× Ohta, Takeshi

WEKO 29112

Ohta, Takeshi

Search repository
Ageta, Yutaka

× Ageta, Yutaka

WEKO 29113

Ageta, Yutaka

Search repository
権利
権利情報 This is a preprint of an article published in HYDROLOGICAL PROCESSES. v.21, 2008, p.2882-2891http://www.interscience.wiley.com/
キーワード
主題Scheme Other
主題 glacier
キーワード
主題Scheme Other
主題 runoff
キーワード
主題Scheme Other
主題 model
キーワード
主題Scheme Other
主題 Tibet
キーワード
主題Scheme Other
主題 climatic sensitivity
キーワード
主題Scheme Other
主題 albedo
抄録
内容記述 Model calculations are made in order to understand the characteristics and response to climate change of runoff from a cold glacier on the Tibetan Plateau. Some 20% of meltwater is preserved at the snow.ice boundary due to refreezing, since the glaciers in mid to northern Tibet are sufficiently cooled during the previous winter. Sensitivity to alterations in meteorological parameters has revealed that a change in air temperature would cause not only an increase in melting by sensible heat, but also a drastic increase in melting due to lowering of the albedo, since some of the snowfall changes to rainfall. In addition, it was suggested that a decrease in precipitation would cause a lowering of the surface albedo, with a resulting increase in the contribution of glacier runoff to the total runoff of river water. This study shows the first quantitative evaluation of the above effects, though they have been suggested qualitatively. The seasonal sensitivity of glacier runoff was examined by changing the dates given for a meteorological perturbation for a period of only 5 days. It was revealed that changes in both air temperature and precipitation during the melting season strongly affected glacier runoff by changing the surface albedo, though these perturbations only slightly altered the annual averages.
内容記述タイプ Abstract
出版者
出版者 Wiley
言語
言語 eng
資源タイプ
資源タイプresource http://purl.org/coar/resource_type/c_6501
タイプ journal article
ISSN
収録物識別子タイプ ISSN
収録物識別子 08856087
書誌情報 HYDROLOGICAL PROCESSES

巻 21, p. 2882-2891, 発行日 2007
フォーマット
application/pdf
著者版フラグ
値 author
URI
識別子 http://hdl.handle.net/2237/11361
識別子タイプ HDL
戻る
0
views
See details
Views

Versions

Ver.1 2021-03-01 11:57:03.441625
Show All versions

Share

Mendeley CiteULike Twitter Facebook Print Addthis

Cite as

Export

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

Confirm


Powered by CERN Data Centre & Invenio


Powered by CERN Data Centre & Invenio