期刊
GEOPHYSICAL RESEARCH LETTERS
卷 35, 期 20, 页码 -出版社
AMER GEOPHYSICAL UNION
DOI: 10.1029/2008GL035319
关键词
-
资金
- German Research Foundation (DFG)
Mineral dust radiative effects and feedbacks upon Saharan boundary layer meteorology are estimated by means of regional dust simulations for a one-week period in May 2006. The regional dust model system LM-MUSCAT is used, which allows online interaction of the computed dust load with the solar and thermal radiation and consequently with the model dynamics. For the Bode le depression, a mechanism is proposed that describes positive and negative dust radiative feedbacks on surface wind speeds and dust emission in dependence on atmospheric stratification, dust-induced stabilization, and baroclinity. These effects are attributed to the formation and breakdown of the low-level jet (LLJ), which is a common phenomenon in the Bodele. However, such processes are likely also relevant for other Saharan regions. Citation: Heinold, B., I. Tegen, K. Schepanski, and O. Hellmuth (2008), Dust radiative feedback on Saharan boundary layer dynamics and dust mobilization, Geophys. Res. Lett., 35, L20817, doi:10.1029/2008GL035319.
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