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Evaluation of Reanalysis Data Based on the Three-dimensional High-density Sounding Data of the Qinghai-Tibet Plateau

机译:基于青藏高原三维高密度探测数据的再分析数据评价

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Based on the data of the third Qinghai-Tibet Plateau atmospheric science experiment from 2015 to 2017,the applicability of plateau weather systems and meteorological elements of two commonly used reanalysis data(NCEP/NCAR reanalysis data set,and ERA-Interim reanalysis data set)in the plateau was evaluated.Some conclusions are obtained as follows.Compared with EC reanalysis data,NCEP reanalysis data are more consistent with the scientific experimental data.The correlation of geopotential height is above 0.99,followed by temperature;The correlation of specific humidity is the worst.Seen from average deviation,geopotential height and temperature are both lower;for EC,the westerly and southerly winds are both weaker;for NCEP,westerly wind is weaker,while southerly wind is stronger;specific humidity is higher.From the perspective of monthly and seasonal distribution characteristics,the average deviation of geopotential height is larger in spring and summer,and that of temperature is slightly worse in late spring and early summer.In terms of wind field,EC deviation is more obvious in winter,while NCEP deviation is more obvious in late spring and early summer.Seen from spatial distribution,the deviations of geological height and temperature in the north of the plateau are smaller than those in the south of the plateau.For wind field,the westerly wind in the Qaidam Basin is weaker,and the southerly wind in the southern plateau is weaker.In vertical profile,the deviation of geopotential height at high levels is greater than that of low levels.The deviation of temperature and wind field is larger near the ground.The temperature at middle levels and the westerly wind at middle and high levels are smaller,and southerly wind is stronger for NCEP.The establishment of the three sounding stations(Gaize,Shenzha and Shiquanhe)is conducive to the discovery of plateau vortex and plateau shear line in the western plateau.The western plateau vortex and plateau shear line mostly appeared in the flood season.Most plateau weather systems were maintained within 24 h,and mainly appeared and disappeared in situ.The objective recognition rate of EC for plateau weather systems is higher than NCEP,so EC is more conducive to the diagnosis and analysis of evolution characteristics of plateau weather systems.
机译:基于2015年至2017年第三次青藏高原大气科学实验的数据,高原天气系统的适用性和两种常用的再分析数据的气象元素(NCEP / NCAR再分析数据集,ERA-Interim Reanalysis数据集)在高原的评估中..获得如下的结论。随着EC再分析数据,NCEP再分析数据与科学实验数据更一致。地理位能高度的相关性高于0.99,其次是温度;特定湿度的相关性;特定湿度的相关性从平均偏差,地理调谐高度和温度都较低;对于EC,西方和南风风均较弱;对于NCEP,Westerly风在较弱,而南风风更强大;特定的湿度更高。从角度来看每月和季节性分布特征,春季和夏季地理势高度的平均偏差较大,温度略微y更糟糕的是在春天和初夏。风场的条款,EC偏差在冬季更加明显,而NCEP偏差在春季和初夏更加明显。从空间分布中,地质高度和温度的偏差高原北方比高原南部的北方。对于风领域,柴达木盆地的西风风较弱,南高原的南风风较弱。在垂直型材,地球势高度偏差高水平大于低水平的水平。温度和风力场的偏差在地面附近更大。中间水平的温度和中高水平的温度较小,NCEP的南风风更强烈。建立在三站(Gaize,Shenzha和Shiquanhe)中有利于西部高原的高原涡旋和高原剪切线。西部高原涡旋和高原剪切线主要出现在洪水季节。大多数高原天气系统在24小时内保持,主要出现并原位消失。高原天气系统的EC的客观识别率高于NCEP,因此EC更有利于进化的诊断和分析高原天气系统的特点。

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