The roles of channels and hillslopes in rainfall/run-off lag times during intense storms in a steep catchment-Reference-Cited by-同舟云学术

The roles of channels and hillslopes in rainfall/run-off lag times during intense storms in a steep catchment

Published:2018-03-12 Issue:6 Volume:32 Page:713-728
ISSN:0885-6087
Container-title:Hydrological Processes
language:en
Short-container-title:Hydrological Processes

Author:

Asano Yuko¹^ORCID,Uchida Taro²

Affiliation:

1. The University of Tokyo Forests, Graduate School of Agricultural and Life Sciences, The University of Tokyo; Japan

2. National Institute for Land and Infrastructure Management; Japan

Funder

Foundation of River & Basin Integrated Communications, Japan

JSPS KAKENHI

Publisher

Wiley

Subject

Water Science and Technology

Reference60 articles.

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2. Flowpath depth is the main controller of mean base flow transit times in a mountainous catchment;Asano;Water Resources Research,2012

3. Detailed documentation of dynamic changes in flow depth and surface velocity during a large flood in a steep mountain stream;Asano;Journal of Hydrology,2016

4. Measured channel resistance at mountain rivers during flood;Asano;Journal of the Japan Society of Erosion Control Engineering,2018

5. Assessing soil stratification using a knocking pole test at the Aono Experimental Forest in the Arboricultural Research Institute;Asano;Enshurin (The University of Tokyo).,2006

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