鉛直不飽和浸透に基づく新しい洪水流出モデルの適用による山地小流域の流出機構の再検討
Author:
Affiliation:
1. Former Graduate School of Agriculture, Kyoto University
Publisher
Japan Society of Hydrology and Water Resources
Subject
Media Technology
Link
https://www.jstage.jst.go.jp/article/jjshwr/36/1/36_36.1741/_pdf
Reference95 articles.
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3. Asano Y, Uchida T, Tomomura M. 2020. A novel method of quantifying catchment-wide average peak propagation speed in hillslopes: Fast hillslope responses are detected during annual floods in a steep humid catchment. Water Resources Research 56, e2019WR025070. DOI: 10.1029/2019WR025070.
4. Beven K, Germann P. 2013. Macropores and water flow in soils revisited. Water Resources Research 49: 3071-3092. DOI: 10.1002/wrcr.20156.
5. Beven K, Kirkby M. 1979. A physically based, variable contributing area model of basin hydrology. Hydrological Sciences Bulletin 24: 43-69. DOI: 10.1080/02626667909491834.
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