Experimental assessment of Owen's second hypothesis on surface shear stress induced by a fluid during sediment saltation-Reference-Cited by-同舟云学术

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Experimental assessment of Owen's second hypothesis on surface shear stress induced by a fluid during sediment saltation

Published:2014-09-03 Issue:17 Volume:41 Page:6298-6305
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Walter B.¹²,Horender S.¹³,Voegeli C.¹⁴,Lehning M.¹⁵

Affiliation:

1. WSL Institute for Snow and Avalanche Research (SLF); Davos Switzerland

2. Physikalisch-Meteorologisches Observatorium Davos (PMOD)/World Radiation Center (WRC); Davos Switzerland

3. Leibniz-Institut für Troposphärenforschung; Leipzig Germany

4. Department of Environmental Systems Science; Swiss Federal Institute of Technology (ETH); Zürich Switzerland

5. CRYOS, School of Architecture, Civil, and Environmental Engineering; École Polytechnique Fédéral de Lausanne (EPFL); Lausanne Switzerland

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1002/2014GL061069/fullpdf

Reference28 articles.

1. Simulation of eolian saltation;Anderson;Science,1988

2. Aeolian sediment transport over vegetation canopies: A wind tunnel study with live plants;Burri;Aeolian Res.,2011

3. Jump at the Onset of Saltation;Carneiro;Phys. Rev. Lett.,2011

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