Sources of Asian dust and role of climate change versus desertification in Asian dust emission

被引:449
作者
Zhang, XY
Gong, SL
Zhao, TL
Arimoto, R
Wang, YQ
Zhou, ZJ
机构
[1] Chinese Acad Sci, Inst Earth Environm, Xian 710075, Peoples R China
[2] Meteorol Serv Canada, Air Qual Res Branch, Toronto, ON M3H 5T4, Canada
[3] New Mexico State Univ, Carlsbad Environm Monitoring & Res Ctr, Carlsbad, NM USA
[4] China Meteorol Adm, Natl Climat Ctr, Beijing 100081, Peoples R China
关键词
D O I
10.1029/2003GL018206
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Simulations of Asian dust emissions over the past 43 years are presented based on a size-dependent soil dust emission and transport model (NARCM) along with supporting data from a network of surface stations. The deserts in Mongolia and in western and northern China (mainly the Taklimakan and Badain Juran, respectively) contribute similar to70% of the total dust emissions; non-Chinese sources account for similar to40% of this. Several areas, especially the Onqin Daga sandy land, Horqin sandy land, and Mu Us Desert, have increased in dust emissions over the past 20 years, but efforts to reduce desertification in these areas may have little effect on Asian dust emission amount because these are not key sources. The model simulations indicate that meteorology and climate have had a greater influence on the Asian dust emissions and associated Asian dust storm occurrences than desertification.
引用
收藏
页码:ASC8 / 1
页数:4
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