Three-dimensional acoustic propagation effect in subaqueous sand dune field

2014 ◽  
Vol 136 (4) ◽  
pp. 2178-2178
Author(s):  
Andrea Y. Chang ◽  
Chi-Fang Chen ◽  
Linus Y. Chiu ◽  
Emily Liu ◽  
Ching-Sang Chiu ◽  
...  
2016 ◽  
Vol 8 (3) ◽  
pp. 434-442
Author(s):  
Jing Wu ◽  
Jianqiang Qian ◽  
Xianzhang Hou ◽  
Carlos A. Busso ◽  
Zhimin Liu ◽  
...  

1995 ◽  
Vol 97 (5) ◽  
pp. 3258-3258 ◽  
Author(s):  
Wayne R. Lundberg

2014 ◽  
Vol 33 (3) ◽  
pp. 199-204 ◽  
Author(s):  
Elwira Żmudzka ◽  
Dariusz Woronko ◽  
Maciej Dłużewski

Abstract Climatic and meteorological conditions may limit the aeolian transport within barchans. An explanation of that issue was the main goal of the investigation held in Western Sahara dune fields located around Tarfaya and Laâyoune. Particular attention was paid to the factors causing the moisture content rising of the sand dune surface layer, which could influence the wind threshold shear velocity in the aeolian transport. The wetted surface layer of sand, when receiving moisture from precipitation or suspensions, reduces the aeolian transport, even in case of wind velocity above 4-5 m s-1. Fog and dew condensation does not affect the moisture of deeper sand layers, what occurs after rainfall.


2005 ◽  
Vol 118 (2) ◽  
pp. 723-734 ◽  
Author(s):  
Scott D. Frank ◽  
Mohsen Badiey ◽  
James F. Lynch ◽  
William L. Siegmann

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