摘要
利用一个耦合了沙尘模型的区域气候模式RegCM3和NCEP再分析资料,对近10年(2000-2009年)东亚地区沙尘气溶胶(直径≤20μm)时空分布特征和起尘通量进行了数值模拟。结果表明,(1)耦合模式能较好地模拟东亚地区沙尘气溶胶的时空分布特点。东亚地区沙尘气溶胶光学厚度、柱含量高值区主要位于塔克拉玛干沙漠和巴丹吉林沙漠。沙尘气溶胶柱含量的季节变化特征明显,春季最大,冬季次之,秋季最小。东亚地区110°E以东,沙尘主要以700hPa高度为中心向东传输。(2)东亚地区起沙源区主要位于塔克拉玛干沙漠、巴丹吉林沙漠、藏北沙漠化地区及蒙古国西南部,起沙强度存在明显的季节变化。2000-2009年东亚地区年平均起沙通量为1015.34mg.m-2.d-1,其中62.4%和2.3%分别通过干、湿过程重新沉降在东亚地区,其余35.3%被净释放进入大气或进行远距离传输。
A regional climate model RegCM3 coupled with an on-line sandy dust module is used to sim- ulate the dust aerosol （smaller than 20μm in diameter） over East Asia in the latest decade from 2000 to 2009. The model is driven by NCEP re-analysis data. Based on the simulation results, the spatial and tem- poral distributions of sandy dust aerosol over East Asia are discussed, and the dust emission flux is also calculated. The model capability to simulate sandy dust aerosol is firstly validated. The simulation results show that the model can capture the characteristics of spatial and temporal distributions of dust aerosol very well over East Asia. There always exist two extremes of dust aerosol optical depth and column bur- den, one is in the Taklimakan Desert of Xinjiang Uygur Autonomous Region, China, and the other is in the Badain Juran Desert of Inner Mongolian Autonomous Region, China. The seasonal variation character istic is evident, with the maximum value appears in spring, the secondary maximum in winter and the minimum in autumn. To the east of 110°E, the dust is transported eastward from a maximum center at a height of 700 hPa over East Asia. The dust emission sources are mainly located in the Taklimakan Desert, Badain Juran Desert, North Qinghai-Xizang Plateau and Southwest Mongolia. There is also an evident sea- sonal variation of dust emission flux. The annual mean dust emission flux is 1015.34 mg·m 2·d-1 , of which 62. 4% and 2. 3% are re-deposited onto continent of East Asia through dry and wet deposition process, respectively, and the remaining 35.3% is injected into the atmosphere or subject to long-range transport.
出处
《高原气象》
CSCD
北大核心
2012年第3期676-687,共12页
Plateau Meteorology
基金
国家重点基础研究发展计划项目(973计划)(2011CB403202)
国家自然科学基金项目(40675040)共同资助
