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  1. B300 農学部/生命農学研究科
  2. B300a 雑誌掲載論文
  3. 学術雑誌

An observational study of the factors that influence interception loss in boreal and temperate forests

http://hdl.handle.net/2237/6939
http://hdl.handle.net/2237/6939
50f26c5e-3525-4030-af86-9bc4a999ee27
名前 / ファイル ライセンス アクション
HYDROL_3204_all.pdf HYDROL_3204_all.pdf (228.2 kB)
Item type 学術雑誌論文 / Journal Article(1)
公開日 2006-09-13
タイトル
タイトル An observational study of the factors that influence interception loss in boreal and temperate forests
言語 en
著者 Toba, T.

× Toba, T.

WEKO 13619

en Toba, T.

Search repository
Ohta, T.

× Ohta, T.

WEKO 13620

en Ohta, T.

Search repository
アクセス権
アクセス権 open access
アクセス権URI http://purl.org/coar/access_right/c_abf2
キーワード
主題Scheme Other
主題 interception loss
キーワード
主題Scheme Other
主題 rainfall characteristics
キーワード
主題Scheme Other
主題 forest structure
キーワード
主題Scheme Other
主題 boreal and temperate
キーワード
主題Scheme Other
主題 energy budget
抄録
内容記述 This study used same methods to observe interception loss in two boreal forest sites in Siberia and five temperate forest sites in Japan; interception characteristics of the two climate regions were compared. The Siberian sites had high interception ratios of 0.2.0.3. In contrast, the Japanese sites had low interception ratios of ca. 0.15 in coniferous forests and 0.2 in broadleaf forests. Although interception loss generally increases with the plant area index (PAI), our data showed the opposite trend. This suggests that meteorological variables had a greater effect on interception loss than did differences in canopy structure. Rainfall characteristics appeared to be the main meteorological factor affecting interception loss. When mean rainfall intensity exceeded 1 mm hr-1, the interception ratio remained near the upper limit of 0.2 regardless of other rainfall conditions. In contrast, windy and drier atmospheric conditions strongly affected the interception rate when the rainfall intensity dropped below 1 mm hr-1. Japan and Siberia showed significant energy-balance differences related to evaporation from wet canopies. At the Siberian sites, the net all-wave radiation was always larger than the latent heat flux used for interception loss, while Japanese sites often showed the opposite pattern. When the latent heat flux exceeded the net all-wave radiation, the air temperature above the canopy during rainfall events was higher at upper levels than at lower levels, even in the daytime. These results indicate that the sensible heat flux was directed downward and suggest that both net all-wave radiation and sensible heat flux contribute to evaporation from wet canopies during and shortly after rainfall events in Japan.
言語 en
内容記述タイプ Abstract
出版者
言語 en
出版者 Elsevier
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
出版タイプ
出版タイプ VoR
出版タイプResource http://purl.org/coar/version/c_970fb48d4fbd8a85
DOI
関連タイプ isVersionOf
識別子タイプ DOI
関連識別子 https://doi.org/10.1016/j.jhydrol.2005.03.003
書誌情報 en : Journal of Hydrology

巻 313, 号 3-4, p. 208-220, 発行日 2005-11
フォーマット
application/pdf
著者版フラグ
値 publisher
URI
識別子 http://hdl.handle.net/2237/6939
識別子タイプ HDL
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