Doi.org/10.1029/2011JF002065
Revision as of 03:52, 18 August 2022 by 187.21.138.9 (talk) (Created page with "== Target Article == Role of pore pressure gradients in sustaining frontal particle entrainment in eruption currents: The case of powder snow avalanches; Louge, M. Y., C. S. Carroll, and B. Turnbull; Journal of Geophysical Research: Earth Surface; 2011; https://doi.org/10.1029/2011JF002065 == Article providing comments == 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 sustain...")
Target Article[edit | edit source]
Role of pore pressure gradients in sustaining frontal particle entrainment in eruption currents: The case of powder snow avalanches; Louge, M. Y., C. S. Carroll, and B. Turnbull; Journal of Geophysical Research: Earth Surface; 2011; https://doi.org/10.1029/2011JF002065
Article providing comments[edit | edit source]
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; COMMENTARY; Bartelt, Perry; Buser, Othmar; ; Journal of Geophysical Research: Earth Surface; 2012-6-01 https://doi.org/10.1029/2012jf002333
Summary[edit | edit source]
Note: Opened to append information.