Late-time drainage from a sloping Boussinesq aquifer-Reference-Cited by-同舟云学术

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Late-time drainage from a sloping Boussinesq aquifer

Published:2013-11 Issue:11 Volume:49 Page:7498-7507
ISSN:0043-1397
Container-title:Water Resources Research
language:en
Short-container-title:Water Resour. Res.

Author:

Bogaart Patrick W.¹,Rupp David E.²,Selker John S.³,van der Velde Ype¹

Affiliation:

1. Copernicus Institute of Sustainable Development; Environmental Sciences group Utrecht University; Utrecht Netherlands

2. Oregon Climate Change Research Institute; College of Earth, Ocean, and Atmospheric Sciences Oregon State University; Corvallis Oregon USA

3. Department of Biological and Ecological Engineering; Oregon State University; Corvallis Oregon USA.

Funder

NWO (Netherlands Organization for Scientific Research) project

Publisher

American Geophysical Union (AGU)

Subject

Water Science and Technology

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1002/2013WR013780/fullpdf

Reference34 articles.

1. Theoretical and conceptual models of subsurface hillslope flows;Basha;Water Resour. Res.,2005

2. Kinematic subsurface stormflow;Beven;Water Resour. Res.,1981

3. A physically based, variable contributing area model of basin hydrology;Beven;Hydrol. Sci. J.,1979

4. Geomorphological origin of recession curves;Biswal;Geophys. Res. Lett.,2010

5. Evaporation into the Atmosphere

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