Timescale dependence of aeolian sand flux observations under atmospheric turbulence
The transport of sand in saltation is driven by the persistently unsteady stresses exerted by
turbulent winds. Based on coupled high‐frequency observations of wind velocity and sand …
turbulent winds. Based on coupled high‐frequency observations of wind velocity and sand …
Aeolian dune field geomorphology modulates the stabilization rate imposed by climate
TE Barchyn, CH Hugenholtz - Journal of Geophysical …, 2012 - Wiley Online Library
The activity of inland aeolian dune fields is typically related to the external forcing imposed
by climate: active (bare) dunes are associated with windy and/or arid settings, and inactive …
by climate: active (bare) dunes are associated with windy and/or arid settings, and inactive …
Predictability of dune activity in real dune fields under unidirectional wind regimes
TE Barchyn, CH Hugenholtz - Journal of Geophysical …, 2015 - Wiley Online Library
We present an analysis of 10 dune fields to test a model‐derived hypothesis of dune field
activity. The hypothesis suggests that a quantifiable threshold exists for stabilization in …
activity. The hypothesis suggests that a quantifiable threshold exists for stabilization in …
Deviations from self‐similarity in barchan form and flux: The case of the Salton Sea dunes, California
JD Pelletier - Journal of Geophysical Research: Earth Surface, 2013 - Wiley Online Library
Barchans are the type of aeolian dune associated with a relatively uniform wind direction,
incomplete sand coverage of the substrate, and low vegetation cover. Here I present an …
incomplete sand coverage of the substrate, and low vegetation cover. Here I present an …
Multiscale bed form interactions and their implications for the abruptness and stability of the downwind dune field margin at White Sands, New Mexico, USA
JD Pelletier, DJ Jerolmack - Journal of Geophysical Research …, 2014 - Wiley Online Library
The downwind margin of White Sands dune field is an abrupt transition from mobile aeolian
dunes to a dune‐free vegetated surface. This margin is also relatively stable; over the past …
dunes to a dune‐free vegetated surface. This margin is also relatively stable; over the past …