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Implementation of 1D+4D-Var assimilation of precipitation-affected microwave radiances at ECMWF. II: 4D-Var

机译:在ECMWF实施1D + 4D-Var同化降水影响的微波辐射。 II:4D-Var

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This paper presents the operational implementation of a 1D+4D-Var assimilation system of rain-affected satellite observations at ECMWF performed on 28 June 2005. The first part describes the methodology and performance analysis of the 1D-Var retrievalscheme in clouds and precipitation that uses Special Sensor Microwave/Imager (SSM/I) microwave radiance observations for the estimation of total-column water vapour (TCWV). This part describes the technical implementation of the TCWV observations in 4D-Var as well as the impact analysis. The effect of the TCWV observations implied by precipitation on the 4D-Var analyses is significant and the total information content is comparable to that of the SSM/I, High-resolution InfraRed Sounder and Advanced Microwave Sounding Unit (AMSU-B) radiances. Regions with systematic drying in the analysis persist throughout the forecast while moistening is removed by precipitation after 1-2 days. The corresponding divergence increments reflect the feedback between moisture and dynamics. Forecast evaluation using model analyses exhibits mostly positive relative-humidity forecast scores, in particular at 700 hPa and in the Tropics. Some short-term negative forecast scores are observed for geopotential near 1000 hPa andin the southern hemisphere between days 1-4. Wind scores vary greatly between regions and different forecast lengths. Tropical cyclone tracking forecasts are only slightly affected by a reduced location error spread through the rain assimilation. Comparison to dropsonde observations of wind and temperature shows improvement as does TCWV analysis validation against independent observations from Jason radiometer data. The system has been implemented operationally in June 2005 and will be further developedtowards a direct 4D-Var assimilation of radiances in clouds and precipitation.
机译:本文介绍了2005年6月28日在ECMWF实施的1D + 4D-Var同化雨天卫星观测系统的业务实施情况。第一部分介绍了使用云和降水的1D-Var检索方案的方法和性能分析,特殊传感器微波/成像仪(SSM / I)微波辐射率观测值,用于估算总柱水蒸气(TCWV)。本部分描述了4D-Var中TCWV观测值的技术实施以及影响分析。降水隐含的TCWV观测对4D-Var分析的影响非常显着,总信息量可与SSM / I,高分辨率红外测深仪和高级微波测深仪(AMSU-B)的辐射量相媲美。分析中具有系统性干燥的区域在整个预测过程中将持续存在,而1-2天后通过降水将水分除去。相应的发散增量反映了水分和动力学之间的反馈。使用模型分析进行的预测评估主要表现出相对正湿度的预测得分,尤其是在700 hPa和热带地区。在1-4天之间,对1000 hPa附近和南半球的地势观测到一些短期的负面预测得分。不同地区和不同预报长度的风速得分差异很大。热带气旋跟踪预报仅受降雨同化过程中位置误差减小的影响。与风速和温度的探空仪观测结果相比,TCWV分析验证相对于Jason辐射计数据的独立观测结果显示出改进。该系统已于2005年6月投入运营,并将进一步发展为直接将云层和降水中的4D-Var同化。

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