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近30年青藏高原上空大气温度变化特征
引用本文:王荣英,周顺武,闫巨盛,王莉萍,王颉.近30年青藏高原上空大气温度变化特征[J].高原山地气象研究,2011,31(1):1-5.
作者姓名:王荣英  周顺武  闫巨盛  王莉萍  王颉
作者单位:1. 南京信息工程大学大气科学学院,南京,210044;河北省衡水市气象局,衡水,053000
2. 南京信息工程大学大气科学学院,南京,210044
3. 河北省衡水市气象局,衡水,053000
基金项目:公益性行业(气象)科研专项经费,中国气象局成都高原气象研究所开放实验室基金LPM2008007
摘    要:根据青藏高原地区16个探空站近30a(1979~2008年)的月平均温度资料对该地区高空年、季平均温度演变特征进行了分析。结果表明:(1)高原上空年、季平均温度均具有较高的空间一致性,其中夏季的一致性特征最弱;(2)高原上空250hPa层及以下和50hPa层及以上平均温度的季节变化特征为冬季最冷、夏季最热,100~70hPa层与其相反;(3)近30a来高原地区对流层中上层(500~250hPa)年平均温度是上升的,对流层上层至平流层下层(150hPa层及以上)以降温为主,高层的降温普遍始于1984年,且变冷显著。

关 键 词:青藏高原  高空  温度  时空演变特征

Analysis of Temporal and Spatial Characteristics about Upper-air Temperature over Tibetan Plateau during Last 30 Years
WANG Rongying,ZHOU Shunwu,YAN Jvsheng,WANG Liping,WANG Jie.Analysis of Temporal and Spatial Characteristics about Upper-air Temperature over Tibetan Plateau during Last 30 Years[J].Plateau and Mountain Meteorology Research,2011,31(1):1-5.
Authors:WANG Rongying  ZHOU Shunwu  YAN Jvsheng  WANG Liping  WANG Jie
Institution:1.College of Atmospheric Science,Nanjing University of Information Science &Technology,Nanjing,210044; 2.Hengshui Meteorological Bureau,Hebei Province,Hengshui,053000)
Abstract:The annual and seasonal characteristics about upper-air temperature in Tibetan Plateau are analyzed on the basis of monthly mean radiosonde records of 16 meteorological stations from 1979 to 2008.The results show that the spatial characteristic of annual mean upper-air temperature is high consistent with that of season over Tibetan Plateau,and in summer it is the weakest.Annual and seasonal characteristics of mean upper-air temperature show that January is the coldest and July is the warmest from 500 to 250hPa and from 30 to 20hPa,while it is contrary from 100 to 70hPa.Annual mean temperature from 500 to 250hPa is rising,while that up 150hPa is falling.The falling,dated from 1984,is significant.
Keywords:Tibetan Plateau  upper air  temperature  temporal and spatial characteristics
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