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基于ERA5压力分层气象数据的对流层散射传播斜延迟分析

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针对当前对流层散射湍流数值模型不能有效反映气象环境对对流层散射传播影响的问题,将欧洲中期天气预报中心(ECMWF)的第五代全球大气再分析数据(ERA5)引入基于三维射线追踪方法的高精度对流层散射延迟计算模型,并选择中国青藏高原、华北平原、四川丘陵、云贵山地、陇蒙荒漠和东南沿海6个典型地理区域的12条散射链路,分别使用ERA5月平均压力分层数据(ERA5 MPL)与每小时压力分层数据(ERA5 HPL)2种数据集来计算,分析各链路对流层散射斜延迟在不同地理环境下变化趋势,同时对2种数据集计算的结果进行比较。结果表明,文中给出的对流层散射传播斜延迟的计算方法对于ERA5压力分层气象数据适用性较好,而且在不同链路上2种数据集所求得结果的最大标准差为2。9 m,授时精度相差不超过10 ns。
An Analysis of Troposcatter Propagation Slant Delay Based on ERA5 Pressure Level Meteorological Data
Aimed at the problem that the current numerical model of tropospheric scattering turbulence fails to effectively reflect the influence of the meteorological environment on tropospheric scattering propa-gation,the fifth-generation global climate reanalysis dataset(ERA5)pressure level meteorological data of the European centre for medium-range weather forecasts(ECMWF)is introduced into the high-precision tropospheric scattering delay calculation model,and 12 scattering links in six typical geographical regions of China,i.e.Tibet Plateau,North China Plain,Sichuan hill,Yunnan-Guizhou mountain,Longmeng desert are selected.The ERA5 hourly data on pressure levels(ERA5 MPL)and ERA5 monthly averaged data on pressure levels(ERA5 MPL)are used to calculate and analyze the trend of tropospheric skew delay of each link in different geographical environments respectively,and simultaneously the results of the cal-culation of the two data sets are compared.The results show that the calculation method of troposcatter propagation slant delay given in this paper is suitable for ERA5 pressure level meteorological data,the maximum standard deviation in the results obtained by the two data sets on different links is 2.9 m,and the timing accuracy difference is less than 10 ns.

troposcatterslant delay3D ray tracingERA5 datasetinterpolation and extrapolation

孙浩冉、刘强、胡邓华、张爽

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空军工程大学防空反导学院,西安,710051

对流层散射 斜延迟 RT 3D算法 ERA5数据集 插值与外推

2024

空军工程大学学报
空军工程大学科研部

空军工程大学学报

CSTPCD北大核心
影响因子:0.55
ISSN:2097-1915
年,卷(期):2024.25(6)