Pleistocene paleowind direction change in the Badain Jaran desert and its environmental significance

Qinghua Daxue Xuebao/Journal of Tsinghua University

Volumn 41, Issue 11, 2001, Pages 118-122

  Yan, Mancun ^a   Wang, Guangqian ^a   Li, Baosheng ^a   Dong, Guangrong ^a  

^a TSINGHUA UNIVERSITY   (China)

Author keywords

Atmospheric circulation; Badain Jaran desert; High megadunes; Paleowind direction

Indexed keywords

ADCOCK DIRECTION FINDERS; ATMOSPHERIC MOVEMENTS; EARTH ATMOSPHERE; WIND; WIND EFFECTS;

BADAIN JARAN DESERT; PALEOWIND DIRECTION CHANGE;

ARID REGIONS;

EID: 0035522132     PISSN: 10000054     EISSN: None     Source Type: Journal    
DOI: None     Document Type: Article

References (19)

1. Formation processes of Qinghai-Tibet plateau and classification of Cenozoic climatic change in China
2. Impact of Qinghai-Tibet plateau uplift on its peripheric environment
3. Aspects of atmospheric circulation; the late Pleistoecene (0-950000 yr) record of eolian deposition in the Pacific Ocean
4. Morphology and sediments of the nebraska sand hills in relation to pleistocene winds and the development of Aeolian bedforms
5. The Ordos, Lanshan and Peishan
6. Formation and growth of high megadunes in Badain Jaran desert
7. Dune forms and wind regime
8. Structures of dunes at white sands national monument New Mexico
9. Landscape development and rainfall change in the Badian Jaran desert since approximately 30 ka B.P.
10. Aeolian bedforms - Their development and origins
11. Subsurface old drainage detection and polaeoenvironment analysis using spaceborne radAr images in Alax plateau
12. Landform evolution of the upper reaches of Huanghe river in late Cenozoic era and the upwelling of Qinghai-Tibet plateau
13. About Kunlun-Huanghe movement