Mechanisms limiting the growth of aeolian megaripples

被引:34
作者
Katra, I. [1 ]
Yizhaq, Hezi [2 ]
Kok, Jasper F. [3 ]
机构
[1] Ben Gurion Univ Negev, Dept Geog & Environm Dev, IL-84105 Beer Sheva, Israel
[2] Ben Gurion Univ Negev, Dept Solar Energy & Environm Phys, Midreshet Ben Gurion, Israel
[3] Univ Calif Los Angeles, Dept Atmospher & Ocean Sci, Los Angeles, CA USA
关键词
megaripples; wind tunnel; fluid threshold; impact threshold; saltation; SELF-ORGANIZATION; EOLIAN RIPPLES; WIND RIPPLES; EARTH; MODEL; MARS;
D O I
10.1002/2013GL058665
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Megaripples are distinguished from regular ripples by their larger size and bimodal sediment distribution. The interplay between wind, grain size, and morphology controls their development, but the exact mechanisms that limit the size of megaripples have been unclear. Using wind tunnel experiments, we found two main mechanisms that limit the height of megaripples. The first mechanism is megaripple flattening due to strong enough winds that drive the coarse grains into saltation; the second mechanism is megaripple deflation by impacts of faster saltation grains. In this latter mechanism, the coarse grains are propelled by the impacts of fine saltating grains. The occurrence of both these mechanisms depends on the grain size distribution and increases with both megaripple height and wind speed. Thus, for a given wind environment and grain size distribution, there exists a limit on the size of megaripples, which is determined by these two mechanisms.
引用
收藏
页码:858 / 865
页数:8
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