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Variational Continuous Assimilation of TMI and SSM/I Rain Rates: Impact on GEOS-3 Hurricane Analyses and Forecasts

机译:TMI和SSM / I雨量的变化连续同化:对GEOS-3飓风的影响分析和预报

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This study describes a 1D variational continuous assimilation (VCA) algorithm for assimilating tropical rainfall data using moisture/temperature time-tendency corrections as the control variable to offset model deficiencies. For rainfall assimilation, model errors are of special concern since model-predicted precipitation is based on parameterized moist physics, which can have substantial systematic errors. The authors examine whether a VCA scheme using the forecast model as a weak constraint offers an effective pathway to precipitation assimilation. The particular scheme investigated employs a precipitation observation operator based on a 6-h integration of a column model of moist physics from the Goddard Earth Observing System (GEOS) global data assimilation system (DAS). In earlier studies, a simplified version of this scheme was tested, and improved monthly mean analyses and better short-range forecast skills were obtained. This paper describes the full implementation of the 1DVCA scheme using background and observation error statistics and examines its impact on GEOS analyses and forecasts of prominent tropical weather systems such as hurricanes. Assimilation experiments with and without rainfall data for Hurricanes Bonnie and Floyd show that assimilating 6-h Tropical Rainfall Measuring Mission (TRMM) Microwave Imager (TMI) and Special Sensor Microwave Imager (SSM/I) surface rain accumulations leads to more realistic analyzed storm features and better 5-day storm track prediction and precipitation forecasts. These results demonstrate the importance of addressing model deficiencies in moisture time tendency in order to make effective use of precipitation information in data assimilation.
机译:这项研究描述了一种一维变分连续同化(VCA)算法,该算法使用湿度/温度时间趋势校正作为控制变量来抵消模型缺陷,从而吸收热带降雨数据。对于降雨同化,模型误差尤其重要,因为模型预测的降雨基于参数化的潮湿物理学,而后者可能具有相当大的系统误差。作者检验了使用预测模型作为弱约束的VCA方案是否提供了有效的降水同化途径。所研究的特定方案使用了一个降水观测算子,该算子基于6个小时来自戈达德地球观测系统(GEOS)全球数据同化系统(DAS)的湿物理学柱模型的积分。在较早的研究中,测试了该方案的简化版本,并获得了改进的每月均值分析和更好的短期预测技能。本文使用背景和观测误差统计数据描述了1DVCA方案的完整实施,并考察了其对GEOS分析和预报(如飓风)等重要热带天气系统的影响。邦妮和弗洛伊德飓风的有或没有降雨数据的同化实验表明,同化6小时热带雨量测量任务(TRMM)微波成像仪(TMI)和特殊传感器微波成像仪(SSM / I)的表面雨水积聚可以得出更现实的分析风暴特征以及更好的5天风暴轨迹预测和降水预测。这些结果证明了解决水分时间趋势模型不足的重要性,以便在数据同化中有效利用降水信息。

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