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Morphological response of asymmetric barchan dunes to bimodal winds and the driving mechanism of surface airflow
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DOI:10.1016/j.geomorph.2026.110366.png)
Abstract
En 中文
• Primary wind cause reversed lee-side flow on the short limb; secondary wind diffuse. • Oblique airflow on short limb under both winds, differing only in angle. • Extended limb migrates downwind under primary winds; short limb elongates.
Keywords:
barchan dunes
bimodal winds
surface airflow
morphological response
wind regime
Journal
IF:
3.3
Papers:
8.5K
Citations:
2.8W
