Reply to comment by P. A. Bartelt and O. Buser on “Role of pore pressure gradients in sustaining frontal particle entrainment in eruption currents: The case of powder snow avalanches”-Reference-Cited by-同舟云学术

Reply to comment by P. A. Bartelt and O. Buser on “Role of pore pressure gradients in sustaining frontal particle entrainment in eruption currents: The case of powder snow avalanches”

Published:2012-04-27 Issue:F2 Volume:117 Page:n/a-n/a
ISSN:0148-0227
Container-title:Journal of Geophysical Research: Earth Surface
language:en
Short-container-title:J. Geophys. Res.

Author:

Louge M. Y.,Carroll C. S.,Turnbull B.

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Link

http://www.agu.org/journals/jf/jf1202/2012JF002380/2012JF002380.pdf

Reference11 articles.

1. Powder cloud eruptions-Where is the air reservoir and blow-out motor in the Rankine half-body? Comment on “Role of pore pressure gradients in sustaining frontal particle entrainment in eruption currents: The case of powder snow avalanches” by M. Y. Louge et al.;Bartelt;J. Geophys. Res.,2012

2. Dispersive pressure and density variations in snow avalanches;Buser;J. Glaciol.,2011

3. Model for dense granular flows down bumpy inclines;Louge;Phys. Rev. E,2003

4. On dense granular flows down flat frictional inclines;Louge;Phys. Fluids,2001

5. Role of pore pressure gradients in sustaining frontal particle entrainment in eruption currents: The case of powder snow avalanches;Louge;J. Geophys. Res.,2011

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1. Frontal dynamics of powder snow avalanches;Journal of Geophysical Research: Earth Surface;2013-05-31