中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Activity of Wind-Blown Sand and the Formation of Feathered Sand Ridges in the Kumtagh Desert, China

文献类型:期刊论文

作者Liao, Kongtai1; Qu, Jianjun1; Tang, Jinnian2; Ding, Feng2; Liu, Hujun2; Zhu, Shujuan2
刊名BOUNDARY-LAYER METEOROLOGY
出版日期2010-05-01
卷号135期号:2页码:333-350
关键词Aeolian geomorphology Blown sand transport Dune evolution Feathered sand ridges
ISSN号0006-8314
DOI10.1007/s10546-010-9469-0
通讯作者Liao, Kongtai(kongtail@163.com)
英文摘要We study the activity of wind-blown sand and its effects on the evolution of feathered sand ridges in the Kumtagh Desert, China, and attempt to reveal the formation process of feathered sand ridges using wind-tunnel experiments, remote sensing data, and detailed field observations from 2005 to 2008. The prevailing wind direction in the Kumtagh Desert is easterly in winter and north-easterly in other seasons. The average annual wind speed is 5.9 ms(-1), and winds sufficiently strong to entrain sand occur on 143 days per annum. The sand transport rate within 0.4 m of the ground is strongly influenced by local landforms, and is related to wind speed by a power function. Wind erosion occurs on the crest, the windward slope of crescent sand ridges and inter-ridge sand strips, where the blowing sand cloud is in an unsaturated state; in contrast, sand accumulation occurs on the leeward slope of the crescent sand ridges, where the blowing sand cloud is in an over-saturated state. These results indicate that the development of feathered sand ridges in the Kumtagh Desert is mainly controlled by the local wind regime. The dominant winds (from the north, north-north-east and north-east) and additional winds (from the east-north-east, east and east-south-east) determine the development of crescent sand ridges, but winds that are approximately parallel to sand ridges form the secondary inter-ridge sand strips.
收录类别SCI
WOS关键词AIR-FLOW ; DUNES ; FIELD ; FLUX ; SEA
WOS研究方向Meteorology & Atmospheric Sciences
WOS类目Meteorology & Atmospheric Sciences
语种英语
WOS记录号WOS:000276709400009
出版者SPRINGER
URI标识http://www.irgrid.ac.cn/handle/1471x/2556323
专题寒区旱区环境与工程研究所
通讯作者Liao, Kongtai
作者单位1.Chinese Acad Sci, Cold & Arid Reg Environm & Engn Res Inst, Lanzhou 730000, Peoples R China
2.Gansu Desert Control Res Inst, Wuwei 733000, Gansu, Peoples R China
推荐引用方式
GB/T 7714
Liao, Kongtai,Qu, Jianjun,Tang, Jinnian,et al. Activity of Wind-Blown Sand and the Formation of Feathered Sand Ridges in the Kumtagh Desert, China[J]. BOUNDARY-LAYER METEOROLOGY,2010,135(2):333-350.
APA Liao, Kongtai,Qu, Jianjun,Tang, Jinnian,Ding, Feng,Liu, Hujun,&Zhu, Shujuan.(2010).Activity of Wind-Blown Sand and the Formation of Feathered Sand Ridges in the Kumtagh Desert, China.BOUNDARY-LAYER METEOROLOGY,135(2),333-350.
MLA Liao, Kongtai,et al."Activity of Wind-Blown Sand and the Formation of Feathered Sand Ridges in the Kumtagh Desert, China".BOUNDARY-LAYER METEOROLOGY 135.2(2010):333-350.

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来源:寒区旱区环境与工程研究所

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