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Evolution and Frontogenesis of an Imbalanced Flow —the Influence of Vapor Distribution and Orographic Forcing
作者姓名:Wang Yunfeng  Wu Rongsheng  Pan Yinong
摘    要:

收稿时间:7 June 1999

Evolution and frontogenesis of an imbalanced flow —the influence of vapor distribution and orographie forcing
Wang Yunfeng,Wu Rongsheng,Pan Yinong.Evolution and frontogenesis of an imbalanced flow —the influence of vapor distribution and orographie forcing[J].Advances in Atmospheric Sciences,2000,17(2):256-274.
Authors:Wang Yunfeng  Wu Rongsheng and Pan Yinong
Institution:Laboratory of Mesoscale Severe Weather, Nanjing University, Nanjing 210093,Laboratory of Mesoscale Severe Weather, Nanjing University, Nanjing 210093,Laboratory of Mesoscale Severe Weather, Nanjing University, Nanjing 210093
Abstract:If the initial fields are not in geostrophic balance, the adjustment and evolution will occur in the stratified fluid, and the frontogenesis will occur under suitable conditions. The evolution is studied here with a nonhydrostatic fully compressible meso-scale model (Advanced Regional Prediction System, ARPS). Four cases are designed and compared: (i) control experiment; (ii) with different initial temperature gradient; (iii) with vapor distribution; (iv) with orographic forcing. The results show that: (1) there is an inertial oscillation in the evolution of the imbalanced flow with the frequency of the local Coriolis f, and with its amplitude de-creasing with time. The stationary balanced state can only be approached as it cannot be reached in the limit duration of time, The energy conversion ratio varies in the range of 0, 1 / 3]; (2) the stronger initial tempera-ture gradient can make the final energy conversion ratio higher, and vice versa; (3) suitable vapor distribu-tion is favorable for the frontogenesis. It will bring forward the time of the frontogenesis, strengthen the in-tensity of the cold front, and influence the final energy conversion ratio; (4) the orographic forcing has an ev-idently strengthening effect on the frontogenesis. The strengthening effect on the frontogenesis and the influ-ence on the final energy conversion ratio depend on the relative location of the mountain to the cold front.
Keywords:Evolution  Frontogenesis  Inertial oscillation  Vapor distribution and orographic forcing
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