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《Chinese Journal of Atmospheric Sciences》 2001-03
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Thermal Adaptation, Overshooting, Dispersion, and Subtropical Anticyclone Part Ⅱ: Horizontal Inhomogeneous Heating and Energy Dispersion

Liu Yimin, Wu Guoxiong, Yu Rucong and Liu Xin (Stale Key Laboratory of Numerical Modeling Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029)  
Based upon potential vorticity theory and thermal adaptation principle, the feature of atmospheric motion as a result of spatial inhomogeneous diabatic heating is investigated. It is further clarified that, due to the variation of the vertical gradient of strong convective condensation heating, the distribution of cyclone and anticyclone in upper troposphere is out of phase with that in the middle and lower the troposphere. On the basis of these results, the impacts of horizontal inhomogeneous heating on the circulation are discussed. It is shown that to the north of a heating region, although there is no diabatic heating, there still exists deep negative vorticity forcing due to the horizontal inhomogeneous in the westerly flow. Air convergence in the low level and divergence in the upper level are induced. This generates ascent as well as negative vorticity source, which corresponds to a strongly anomaly anticyclone center appearing to the north of the heating region. This negative vorticity source can propagate in the westerly flow through energy dispersion and affect the circulation in mid-high latitudes.
【Fund】: 国家重点基础研究发展规划项目!G1998040900;; 中国科学院“百人计划”气候模式的有效化;; 国家自然科学基金!4990500
【CateGory Index】: P433
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