Dynamic runoff connectivity of overland flow on steep forested hillslopes: Scale effects and runoff transfer-Reference-Cited by-同舟云学术

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Dynamic runoff connectivity of overland flow on steep forested hillslopes: Scale effects and runoff transfer

Published:2008-08 Issue:8 Volume:44 Page:
ISSN:0043-1397
Container-title:Water Resources Research
language:en
Short-container-title:Water Resour. Res.

Author:

Gomi Takashi¹,Sidle Roy C.²,Miyata Shusuke³,Kosugi Ken'ichirou³,Onda Yuichi⁴

Affiliation:

1. Department of International Environmental and Agriculture Science; Tokyo University of Agriculture and Technology; Tokyo Japan

2. Geohazards Division, Disaster Prevention Research Institute; Kyoto University; Kyoto Japan

3. Laboratory of Erosion Control, Division of Forest and Biomaterial Science, Graduate School of Agriculture; Kyoto University; Kyoto Japan

4. Department of Integrative Environmental Sciences, Graduate School of Life and Environmental Sciences; University of Tsukuba; Tsukuba Japan

Publisher

American Geophysical Union (AGU)

Subject

Water Science and Technology

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1029/2007WR005894/fullpdf

Reference60 articles.

1. Distribution of depth of overland flow on desert hillslopes and its implications for modeling soil erosion;Abrahams;J. Hydrol.,1989

2. Resistance to overland flow on semiarid grassland and shrubland hillslopes, Walnut Gulch, southern Arizona;Abrahams;J. Hydrol.,1994

3. Identification, characterization and hydrological implication of water repellency in mountain soils, southern British Columbia;Barrett;Catena,1989

4. Investigations on the runoff generation at the profile and plot scales, Swiss Emmental;Badoux;Hydrol. Processes,2006

5. Laboratory experiments on the influence of slope length on runoff, percolation and rill development;Bryan;Earth Surf. Processes Landforms,1989

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