A Comparative Analysis of Two Geopotential Height Field Reanalysis Datasets in Plateau
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摘要:
利用ERA40、NCEPI (NCEP/NCAR version I)再分析資料以及高原地區的探空資料和1979年青藏高原地區第1次氣象科學試驗資料,詳細的比較了高原地區位勢高度的特征。結果表明,兩套再分析資料在高原地區具有一定的相似性,但仍存在著明顯的差別。相比較而言,高原北部地區ERA40再分析資料除1980—1990年在200 hPa高層優于NCEPI再分析資料外,NCEPI再分析資料在年際變化上更接近探空資料;高原中部和南部地區NCEPI再分析資料除1980—1990年在200 hPa高層優于ERA40再分析資料外,ERA40再分析資料在年際變化上更接近探空資料。與1979年青藏高原地區第1次氣象科學試驗資料空間相關關系的比較顯示,ERA40再分析資料在空間上與試驗資料更相似。
Abstract:
Based on ERA40 and NCEPI (NCEP/NCAR version I) reanalysis datasets, the upperair observation datasets over the QinghaiXizang Plateau, and the data from the first Tibetan Plateau field experiment in 1979, the characteristics of geopotential heights over the QinghaiXizang Plateau are compared. Although there are some similarities, sensible differences among several reanalysis datasets are found. Comparatively speaking, the deviation of NCEPI reanalysis datasets from upperair observation datasets is the smallest, while that of ERA40 reanalysis datasets is the smallest over 200 hPa from 1980 to 1990 in the northern Plateau. Except that NCEPI reanalysis datasets are in better agreement with the upperair observation datasets over 200 hPa from 1980 to 1990, ERA40 reanalysis datasets are probably closer to reality on the interdecadal timescale in the central and southern Plateau. ERA40 reanalysis datasets show a better spatial similarity to the data from the first Tibetan Plateau field experiment than NCEPI reanalysis datasets.