Wind regimes and associated sand dune types in the hinterland of the Badain Jaran Desert, China

Author:

Meng Nan,Wang Nai’ang,Zhao Liqiang,Niu Zhenmin,Sun Jiaqi

Publisher

Springer Science and Business Media LLC

Subject

Management, Monitoring, Policy and Law,Earth-Surface Processes,Water Science and Technology

Reference61 articles.

1. Al-Awadhi J M, Al-Helal A, Al-Enezi A. 2005. Sand drift potential in the desert of Kuwait. Journal of Arid Environments, 63(2): 425–438.

2. An Z S, Zhang K C, Qu J J, et al. 2014. The near-surface airflow filed of pyramid dune and its influence on the Crescent Moon Spring in Dunhuang, China. Journal of Desert Research, 34(1): 9–15. (in Chinese)

3. Bagnold R A. 1974. The Physics of Blown Sand and Desert Dunes. Dordrecht: Springer, 85–95.

4. Bai Y, Wang N A, Liao K T, et al. 2011. Geomorphological evolution revealed by aeolian sedimentary structure in Badain Jaran Desert on Alxa Plateau, Northwest China. Chinese Geographical Science, 21(3): 267–278.

5. Breed C S, Fryberger S G, Andrews S, et al. 1979. Regional studies of sand seas using landsat (ERTS) imagery. In: McKee E D. A Study of Global Sand Seas. Washington: United States Geological Survey, 305–397.

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