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丘陵山区低空急流特性分析
引用本文:郝为锋,王庆安.丘陵山区低空急流特性分析[J].气象科学,1996,16(3):256-263.
作者姓名:郝为锋  王庆安
作者单位:空军气象学院!21110(郝为锋),南京大学大气科学系!210008(王庆安),空军气象学院!211101(苏晓冰,邹爱生)
摘    要:利用丘陵区边界层实测资料,分析了该地区8-9月份低空急流的特征及其演变规律;并从测站所处的地理环境,山凰 地形的力差异以及适中的风平流作用等,探讨了测站上空逆温的形成及其对低空急流的形成和维持作用,根据地形热力差所导致的气压斜压性,研究了低空急流的生消可能机制。

关 键 词:低空急流  风廓线  斜压性  气流  丘陵区

THE ANALYSIS OF THE CHARACTERISTICS OF LOW-LEVEL-JET(LLJ) IN HILLY AREA
Hao Weifeng.THE ANALYSIS OF THE CHARACTERISTICS OF LOW-LEVEL-JET(LLJ) IN HILLY AREA[J].Scientia Meteorologica Sinica,1996,16(3):256-263.
Authors:Hao Weifeng
Abstract:By using boundary layer data actually measured in hilly area,we analyse the characteristics and evolutional law of LLJ in August and September in that area;on the basis of the geographical environment where the station locates,the thermodynamic difference of hilly terrain,and the effect of medium wind-advection,etc.,we analyse the formation of hanging invertion over the station and its effects on LLJ's formation and maintenance ;according to layer's barocline resulting from terrain' s thermodynamic difference, we explore the possible essence of LLJ's genesis and disappearance.
Keywords:Low level jet  Wind profile  Hanging invertion  Barocline feature  
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