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- W2389359611 abstract "Using the long term monthly mean pressure and monthly mean pressure data on tropopause of NCEP/NCAR reanalysis data,the spatial distributional and temporal evolution of tropopause height over China in recent 51 years are studied by Empirical Orthogonal Function(EOF) and Rotated Empirical Orthogonal Function(REOF) methods.The results show that the boundary line between the tropical tropopause(the second tropopause) and the polar tropopause(the first tropopause) is on the most southern side of China in February and on the most northern side of China in August.The higher tropical tropopause gradually moves too north since February and reaches the north-edge about 44°N in August,and then withdraws southward and reaches the south-edge about 29°~30°N in February.Annual variation amplitude of the tropopause height is greater in the region of 29°~44°N in China.There are three main EOF modes of tropopause height field: The first EOF mode is consistently higher(lower) than normal;the second EOF mode is a opposite pattern between southern(northern) region and northern(southern) region;the third EOF mode is a opposite pattern between northern-southern(central) region and central(northern-southern) region.Furthermore,based on the data of tropopause height field,the studied region can be divided into 6 sub-regions by REOF.They are South China,Xinjiang region,Northeast China,North China,the Yangtze River valley and Tibet Plateau area.The maximum tropopause height generally occurs in summer and the minimum occurs in winter in each region except for South China.In South China,the maximum tropopause height occurs in spring and the minimum occurs in summer.The interannual change and secular trend of the tropopause height show obvious regional differences." @default.
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- W2389359611 date "2012-04-23" @default.
- W2389359611 modified "2023-09-23" @default.
- W2389359611 title "Characteristic of Tropopause Height over China in Recent 51 Years" @default.
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