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祁连山区能量场特征与降水分布的关系分析
引用本文:陈乾,陈添宇,张逸轩.祁连山区能量场特征与降水分布的关系分析[J].冰川冻土,2011,33(5):1046-1054.
作者姓名:陈乾  陈添宇  张逸轩
作者单位:甘肃省人工影响天气办公室,甘肃兰州,730020;重庆市人工影响天气办公室,重庆,401147
基金项目:公益性行业(气象)科研专项(GYHY20090624)资助
摘    要:采用祁连山地形云野外观测的资料,分西南气流移动、西南气流阻塞、西北和平直西风气流型,用三维插值方法分型计算湿静力总温度Tσ场和总降水场,分析了不同的大尺度流型下冷龙岭西段降水分布与能量场特征的关系.对比山脉南北坡与山外同高度Tσ的日变化,发现山坡Tσ全天高于山外,山脉呈高能岛其外围有能量锋,不同流型下南北坡能量锋强度和...

关 键 词:祁连山区  湿静力总温度场  地形云降水

Analyses of Energy Field Characteristics and Precipitation in Qilian Mountains
CHEN Qian,CHEN Tian-yu,ZHANG Yi-xuan.Analyses of Energy Field Characteristics and Precipitation in Qilian Mountains[J].Journal of Glaciology and Geocryology,2011,33(5):1046-1054.
Authors:CHEN Qian  CHEN Tian-yu  ZHANG Yi-xuan
Institution:CHEN Qian1,CHEN Tian-yu1,ZHANG Yi-xuan2(1.Gansu Weather Modification Office,Lanzhou Gansu 730020,China,2.Chongqing Municipality Weather Modification Office,Chongqing 401147,China)
Abstract:In this paper,using observation data of orographic cloud over the Qilian Mountains,the air current was divided into southwest air current moving pattern,southwest air current obstruction pattern,northwest air current pattern and straight westerly pattern.Wet static total temperature T-σ field and total precipitation field have been calculated with three-dimensional interpolation method.For different macro scale circulation pattern,the relation between precipitation distribution and energy field characteristics in the western Lenglong Range has been analyzed.Contrasting the daily variations of T-σ between the north and south slopes of the range and at the same altitude outside the range,it is found that T-σ inside the range is always higher that outside the range,with a high energy island over the range and energy fronts outside the range.Energy front intensity and T-σ vertical profile are very different for different circulation patterns,corresponding to orographic cloud precipitation very well.The daily mean precipitation has maximum negative correlation with convective instability index(ΔT-σ=surface T-σ subtracts T-σ at 500 hPa).However,it has positive correlation with the T-σ averaged from the surface to 300 hPa.One can see that weak convective instability day with high energy has maximum daily precipitation,whereas strong convective instability day with low energy has less precipitation or not.There is not obvious relationship between energy front intensity and daily precipitation.
Keywords:Qilian Mountains  wet static total temperature field  orographic cloud precipitation  
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