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  1. 0 資料タイプ別
  2. 01 学術雑誌論文
  1. 360 災害・復興科学研究所
  2. 10 学術雑誌論文
  3. 10 査読済論文

平成18年豪雪における積雪深分布の特徴

http://hdl.handle.net/10191/9286
http://hdl.handle.net/10191/9286
410cd862-b917-4662-8b7f-3889457afad7
名前 / ファイル ライセンス アクション
69(1)_45-52.pdf 69(1)_45-52.pdf (791.6 kB)
Item type 学術雑誌論文 / Journal Article(1)
公開日 2009-08-07
タイトル
タイトル 平成18年豪雪における積雪深分布の特徴
タイトル
言語 en
タイトル 平成18年豪雪における積雪深分布の特徴
言語
言語 jpn
キーワード
主題Scheme Other
主題 平成18年豪雪
キーワード
主題Scheme Other
主題 積雪深分布
キーワード
主題Scheme Other
主題 高度分布
キーワード
主題Scheme Other
主題 内陸山間部
キーワード
主題Scheme Other
主題 heavy snowfall of 2005-2006 winter
キーワード
主題Scheme Other
主題 snow-depth distribution
キーワード
主題Scheme Other
主題 altitudinal distribution
キーワード
主題Scheme Other
主題 inland mountainous region
資源タイプ
資源 http://purl.org/coar/resource_type/c_6501
タイプ journal article
その他のタイトル
その他のタイトル Characteristics of snow-depth distribution in Japan during heavy snowfall of 2005-2006 winter
著者 伊豫部, 勉

× 伊豫部, 勉

WEKO 40929

伊豫部, 勉

Search repository
河島, 克久

× 河島, 克久

WEKO 40930

河島, 克久

Search repository
和泉, 薫

× 和泉, 薫

WEKO 40931

和泉, 薫

Search repository
著者別名
識別子 40932
識別子Scheme WEKO
姓名 Iyobe, Tsutomu
著者別名
識別子 40933
識別子Scheme WEKO
姓名 Kawashima, Katsuhisa
著者別名
識別子 40934
識別子Scheme WEKO
姓名 Izumi, Kaoru
抄録
内容記述タイプ Abstract
内容記述 平成18年豪雪における積雪深分布を詳細に明らかにすることを目的として,2006年2月6日9:00に多機関で計測された積雪深を全国的に収集した.1917地点のデータを基に日本列島の積雪深分布図の作成を行い,その地域的特徴について調べた.その結果,3mを超える豪雪エリアは日本海側地域の内陸山間部を中心に広がり,なかでも越後三山周辺では5mに達するエリアがみられた.日本海側地域における積雪深の分布には高度依存性がみられたが,標高の増大に伴う積雪深の増加率は南北で異なっていた.山形県および新潟県の積雪深は,標高300m以上の地点で横ばいに分布する傾向がみられ,高標高側ほど根雪期間が長く積雪荷重が大きいため積雪の圧密が促進されることが関与していた.特に新潟県ではこの傾向が他の豪雪年でもみられることから,平成18年豪雪に限定された現象ではないと推察された.同時期の気象庁データ(315地点)を基に作成した積雪深分布図との比較を行ったところ,気象庁データでは山間部の積雪深が1m以上過小評価される傾向がみられ,内陸山間部に偏在化した積雪深分布を正確に把握することが出来ない可能性が示唆された.
抄録
内容記述タイプ Abstract
内容記述 In this paper, we perform a detailed evaluation of the snow-depth distribution in Japan caused by heavy snowfall of 2005-2006 winter. The snow-depth data were investigated according to the values measured all over Japan on February 6, 2006; consequently, 1917 points were collected. Heavy snow areas (depth of over 3m) were found mainly in the inland mountainous regions bordering the Sea of Japan. The highest snow-depth value was 5m around Echigo-Sanzan. The snow depth uniformly increased with an increase in the altitude in all the regions bordering the Sea of Japan; however, the ratios of the increases in the snow depth to the altitude were different. The snow depths in Yamagata and Niigata prefectures remained unchanged at over 300m a.s.l. These results can be attributed to the consolidation of the snowpack as a result of both the high snowfall loading and long duration of snow covering. In the Niigata prefecture, a pattern of peak values was observed at higher altitudes during other heavy snowfall occurrences as well, which implies that such altitudinal distribution of the snow depth was not limited only during the 2005-2006 winter. In the heavy snowfall area located in inland mountainous region, the snow-depth distribution at 315 points (measured by the Japan Meteorological Agency) was estimated to be smaller than the values in our data for a ddepth of above 1m; therefore, it might be impossible to exactly understand the snow-depth distribution including the maldistribution of the snowpacks in inland mountainous regions.
書誌情報 雪氷
en : 雪氷

巻 69, 号 1, p. 45-52, 発行日 2007-01
出版者
出版者 日本雪氷学会
ISSN
収録物識別子タイプ ISSN
収録物識別子 03731006
書誌レコードID
収録物識別子タイプ NCID
収録物識別子 AN00131221
著者版フラグ
値 publisher
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