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作 者:赵林[1,2] 陈玉春[1] 吕世华[1] 李锁锁[1]
机构地区:[1]中国科学院寒区旱区环境与工程研究所西部气候环境与灾害实验室,甘肃兰州730000 [2]中国科学院研究生院,北京100039
出 处:《Meteorological and Environmental Research》2010年第9期67-71,共5页气象与环境研究(英文版)
基 金:Supported by National Science and Technology Support Project(2007BAC29B04);Major State Basic Research Development Program of China(2009CB421402)
摘 要:Using the mesoscale regional atmospheric model RAMS(The Regional Atmospheric Modeling System),the climatic effects of underlying surface vegetation changes of Tibetan Plateau were conducted the numerical simulation.The possible influence of vegetation variation on regional climate was studied.The results showed that the climatic effects of Tibetan Plateau were well represented in the upper troposphere(300 hPa).The heating effect and cooling effect caused by vegetation changes of Tibetan Plateau were inconsistent between land surface and upper air,and the cyclone(anticyclone) differences reflected in the flow field would enhance South Asia high in the higher troposphere(lower southwest vortex system),which might have an effect on the precipitation in Yangtze River basin.Using the mesoscale regional atmospheric model RAMS(The Regional Atmospheric Modeling System),the climatic effects of underlying surface vegetation changes of Tibetan Plateau were conducted the numerical simulation.The possible influence of vegetation variation on regional climate was studied.The results showed that the climatic effects of Tibetan Plateau were well represented in the upper troposphere(300 hPa).The heating effect and cooling effect caused by vegetation changes of Tibetan Plateau were inconsistent between land surface and upper air,and the cyclone(anticyclone) differences reflected in the flow field would enhance South Asia high in the higher troposphere(lower southwest vortex system),which might have an effect on the precipitation in Yangtze River basin.
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