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Development of a coupled land-atmosphere satellite data assimilation system for improved local atmospheric simulations

机译:开发用于改进局部大气模拟的陆地-大气卫星耦合数据同化系统

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This study developed a coupled land-atmosphere satellite data assimilation system as a new physical downscaling approach, by coupling a mesoscale atmospheric model with a land data assimilation system (LDAS). The LDAS consists of a land surface scheme as the model operator, a radiative transfer model as the observation operator, and the simulated annealing method for minimizing the difference between the observed and simulated microwave brightness temperature. The atmospheric model produces forcing data for the LDAS, and the LDAS produces better initial surface conditions for the modelling system. This coupled system can take into account land surface heterogeneities through assimilating satellite data for a better precipitation prediction. To assess the effectiveness of the new system, 3-dimensional numerical experiments were carried out in a mesoscale area of the Tibetan Plateau during the wet monsoon season. The results show significant improvement compared with a no assimilation regional atmospheric model simply nested from the global model. The surface soil moisture content and its distribution from the assimilation system were more consistent to in situ observations. These better surface conditions affect the land-atmosphere interactions through convection systems and lead to better atmospheric predictability as confirmed by satellite-based cloud observations and in situ sounding observations. Through the use of satellite brightness temperature, the developed coupled land-atmosphere assimilation system has shown potential ability to provide better initial surface conditions and its inputs to the atmosphere and to improve physical downscaling through regional models. (C) 2007 Elsevier Inc. All rights reserved.
机译:这项研究通过将中尺度大气模型与土地数据同化系统(LDAS)结合,开发了一种耦合的陆地-大气卫星数据同化系统,作为一种新的物理降尺度方法。 LDAS包括作为模型算子的陆面方案,作为观测算子的辐射传递模型,以及用于使观测到的微波亮度温度与模拟微波亮度温度之间的差异最小的模拟退火方法。大气模型为LDAS生成强迫数据,而LDAS为建模系统生成更好的初始表面条件。该耦合系统可以通过吸收卫星数据来考虑陆地表面的非均质性,以实现更好的降水预测。为了评估新系统的有效性,在季风雨季的中尺度地区进行了三维数值试验。与仅从全局模型嵌套的无同化区域大气模型相比,结果显示出显着改善。同化系统的表层土壤水分含量及其分布与原位观测更为一致。这些更好的地表条件通过对流系统影响了陆地与大气的相互作用,并导致了更好的大气可预测性,这已经通过基于卫星的云观测和原位测深观测得到了证实。通过使用卫星亮度温度,已开发的耦合陆地-大气同化系统已显示出可能提供更好的初始地面条件及其对大气的输入以及通过区域模型改善物理降尺度的潜在能力。 (C)2007 Elsevier Inc.保留所有权利。

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