Health & Environmental Research Online (HERO)


Print Feedback Export to File
2565902 
Journal Article 
Contributions of sandy lands and stony deserts to long-distance dust emission in China and Mongolia during 2000-2006 
Zhang, B; Tsunekawa, A; Tsubo, M 
2008 
Yes 
Global and Planetary Change
ISSN: 0921-8181 
60 
3-4 
487-504 
WOS:000253576900020 
More than 400 Moderate Resolution Imaging Spectroradiometer (MODIS) images of dust storm events were collected and analyzed, and individual events were tracked back to their origins. Dust tracks were determined from color composite images, brightness temperature difference (BTD) and the NOAA Hybrid Single-Particle Lagrangian Integrated Trajectory model. The results showed that five regions (sandy lands in central Inner Mongolia and the adjacent area of Mongolia; the Gobi Desert in Xinjiang and Gansu provinces, western Inner Mongolia, and the adjacent southwestern area of Mongolia; the Gobi Desert in southern Mongolia and the adjoining area of northern Inner Mongolia; sandy lands and deserts around the middle reaches of the Yellow River; and the area rimming the Taklimakan Desert) were the main contributors to long-lived mineral dusts in northern China and Mongolia. Of these dust production areas, sandy lands and stony deserts, rather than the sandy deserts of Inner Mongolia and Mongolia, were found to be the dominant dust sources, accounting for more than 75% of regional dust emission events. Dust events in the Taklimakan Desert were often local phenomena, although they could also be transported eastward if they were uplifted high enough to escape the enclosing topographic highs. Dust sources in northwestern China are mainly alluvial fans and dry lake and river beds. Success in identifying the sources and trajectories of Asian dust storms would guide future ground-based research and steppe degradation countermeasures and help reduce the uncertainties in modem modeling of Asian dust. (c) 2007 Elsevier B.V. All rights reserved. 
dust source; long-range transport; MODIS; HYSPLIT model; brightness temperature difference