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Reanalysis of the Indian summer monsoon: four dimensional data assimilation of AIRS retrievals in a regional data assimilation and modeling framework

机译:印度夏季风的重新分析:区域数据同化和建模框架中AIRS取回的四维数据同化

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摘要

This work is the first attempt to produce a multi-year downscaled regional reanalysis of the Indian summer monsoon (ISM) using the National Centers for Environmental Prediction (NCEP) operational analyses and Atmospheric Infrared Sounder (AIRS) version 5 temperature and moisture retrievals in a regional model. Reanalysis of nine monsoon seasons (2003-2011) are produced in two parallel setups. The first set of experiments simply downscale the original NCEP operational analyses, whilst the second one assimilates the AIRS temperature and moisture profiles. The results show better representation of the key monsoon features such as low level jet, tropical easterly jet, subtropical westerly jet, monsoon trough and the spatial pattern of precipitation when AIRS profiles are assimilated (compared to those without AIRS data assimilation). The distribution of temperature, moisture and meridional gradients of dynamical and thermodynamical fields over the monsoon region are better represented in the reanalysis that assimilates AIRS profiles. The change induced by AIRS data on the moist and thermodynamic conditions results in more realistic rendering of the vertical shear associated with the monsoon, which in turn leads to a proper moisture transport and the moist convective feedback. This feedback benefits the representation of the regional monsoon characteristics, the monsoon dynamics and the moist convective processes on the seasonal time scale. This study emphasizes the use of AIRS soundings for downscaling of ISM representation in a regional reanalysis.
机译:这项工作是首次尝试使用国家环境预测中心(NCEP)运营分析和大气红外测深仪(AIRS)版本5进行的印度夏季风(ISM)的多年缩减规模的区域再分析,区域模型。在两个平行设置中对九个季风季节(2003-2011年)进行了重新分析。第一组实验只是缩小了原始NCEP操作分析的规模,而第二组实验则吸收了AIRS的温度和湿度曲线。结果表明,与AIRS资料同化后,季风关键特征如低空急流,热带东风急流,亚热带西风急流,季风槽和降水的空间格局得到了更好的表示(与没有AIRS资料同化的那些相比)。季风区域内动态和热力学场的温度,湿度和子午线梯度的分布在同化AIRS剖面的重新分析中得到了更好的体现。 AIRS数据在潮湿和热力学条件下引起的变化导致与季风相关的垂直切变更逼真的渲染,进而导致适当的水分传输和潮湿的对流反馈。该反馈有益于在季节时间尺度上表示区域季风特征,季风动力学和潮湿的对流过程。这项研究强调了在区域重新分析中使用AIRS测深来缩小ISM表示的比例。

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