首页> 外文期刊>ournal of the Meteorological Society of Japan >Three-Dimensional Variational Data Assimilation Experiments for a Heavy Rainfall Case in the Downstream Yangtze River Valley Using Automatic Weather Station and Global Positioning System Data in Southeastern Tibetan Plateau
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Three-Dimensional Variational Data Assimilation Experiments for a Heavy Rainfall Case in the Downstream Yangtze River Valley Using Automatic Weather Station and Global Positioning System Data in Southeastern Tibetan Plateau

机译:青藏高原东南部利用自动气象站和全球定位系统数据对长江下游流域的一次大暴雨案例进行三维变分数据同化实验

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 A severe rainfall event occurred in the downstream Yangtze River Valley (YRV) during 28-30 June 2009. This study focused on the role of the “key sensitive area” (KSA) in the southeastern edge of the Tibetan Plateau (TP) in transporting water vapor downstream. The characteristics of water-vapor transport from KSA and the relation with the summer rainfall event were first investigated using the National Centers for Environmental Prediction Final Operational Global Analysis data and conventional observations. The observations included temperature, specific humidity (q), and surface pressure that are all from the automatic weather stations (AWS) over TP; precipitable water vapor (PWV) from the Global Positioning System (GPS) stations over TP; and rainfall from rain gauge measurements in YRV. The results showed high correlations between variables (i.e., q and PWV) observed over KSA and the summer rainfall in YRV, with a lagged time of 48-72 h, suggesting that the former is a good early-warning signal for the latter. To confirm the importance of KSA and its impact on the rainfall in the downstream YRV, the observations from the AWS and GPS of the New Integrated Observational System over TP were assimilated into the Advanced Research Weather Research and Forecast model with 30-km mesh using three-dimensional variational method. A set of sensitivity experiments were also conducted during a different summer, namely, June 2008, and Threat Score is used to evaluate the rainfall forecast skill. The results showed that the assimilation of observations from AWS and GPS in KSA helped adjust the structures of moisture, temperature, and wind fields, which improved the rainfall forecast in YRV, especially the heavy rainfall event. Both data analysis and numerical experiments demonstrated that the observations in KSA improved the forecast of high-impact weather in YRV.
机译:2009年6月28日至30日,长江流域下游发生了一次强降雨事件。该研究的重点是青藏高原东南缘的“关键敏感区”(KSA)在运输中的作用。下游有水蒸气。首先使用国家环境预测中心的最终运行全球分析数据和常规观测资料,研究了来自KSA的水汽输送特征及其与夏季降雨事件的关系。观测值包括温度,比湿度(q)和表面压力,这些都来自TP上的自动气象站(AWS); TP上来自全球定位系统(GPS)站的可沉淀水蒸气(PWV); YRV中雨量计的测量结果和降雨。结果表明,在KSA上观测到的变量(即q和PWV)与YRV的夏季降雨之间存在高度相关性,滞后时间为48-72 h,这表明前者是后者的良好预警信号。为了确认KSA的重要性及其对下游YRV降雨的影响,将新的综合观测系统对TP的AWS和GPS的观测值同化为30 km网格的高级研究天气研究和预报模型,使用三个维变分方法。在另一个不同的夏季(即2008年6月)也进行了一组敏感性实验,并使用“威胁评分”来评估降雨预报技能。结果表明,在KSA中对AWS和GPS的观测结果的同化有助于调整湿度,温度和风场的结构,从而改善了YRV的降雨预报,特别是强降雨事件。数据分析和数值实验均表明,KSA的观测改善了YRV高影响天气的预报。

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