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Radiative transfer calculations for a passive microwave satellite sensor : comparing a fast model and a line-by-line model

机译:无源微波卫星传感器的辐射传输计算:比较快速模型和逐行模型

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摘要

[1] A comparison between the fast radiative transfer model Radiative Transfer for the TIROS Operational Vertical Sounder (RTTOV-7) and the physical radiative transfer model Atmospheric Radiative Transfer Simulator ( ARTS) was carried out. Radiances were simulated for the sounding channels of the Advanced Microwave Sounding Unit B (AMSU-B) for the whole globe for a single time of a single day ( 1 January 2000, 0000 UT). Temperature, pressure, and specific humidity profiles from the reanalysis data set ERA-40 of the European Centre for Medium-Range Weather Forecasts (ECMWF) were used as input for both models; geopotential height profiles were also used but only as input for ARTS. The simulations were made for two different surface emissivities, 0.60 and 0.95. The low surface emissivity case exhibits the larger radiance differences. Although the global values of the mean difference and standard deviation are small ( for example, the global mean difference for channel 18 is 0.014 K and the standard deviation is 0.232 K), the examination of the geographical distribution of the differences shows that large positive or negative values are observed over dry regions of high northern and southern latitudes and over dry elevated regions. The origin of these differences was found to be due to errors introduced by the transmittance parametrization used in RTTOV.
机译:[1]在TIROS操作垂直测深仪(RTTOV-7)的快速辐射传递模型辐射传递与物理辐射传递模型大气辐射传递模拟器(ARTS)之间进行了比较。在一天中的单个时间(2000年1月1日,0000 UT)中模拟了高级微波探测单元B(AMSU-B)在整个地球上的探测通道的辐射。欧洲中距离天气预报中心(ECMWF)的再分析数据集ERA-40的温度,压力和特定湿度曲线被用作两个模型的输入。也使用了地势高度剖面,但仅作为ARTS的输入。针对两种不同的表面发射率0.60和0.95进行了仿真。低表面发射率情况下显示出更大的辐射率差异。尽管平均差异和标准偏差的整体值很小(例如,通道18的整体平均差异为0.014 K,标准偏差为0.232 K),但对差异的地理分布的检查表明,正值或正值较大在北部和南部高纬度的干旱地区以及海拔高的干旱地区,观测到负值。发现这些差异的根源是由于RTTOV中使用的透射率参数化引入的误差。

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