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High-Resolution Radar Data Assimilation For Hurricane Isabel (2003) At Landfall

机译:伊莎贝尔飓风(2003)在登陆时的高分辨率雷达数据同化

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Major damage caused by hurricanes occurs over land during and after landfall. Accurate predictions of winds and precipitation in and around hurricanes at or near landfall are therefore of vital importance for hurricane preparation and damage mitigation, yet they continue to present a challenge for the hurricane research and numerical weather prediction (NWP) communities. This is, in part, due to rapid changes in hurricane intensity and structure during landfall associated with multiscale dynamical and physical interactions in the hurricane core regions and outer spiral rainbands, and also associated with sudden changes of surface conditions. In this study, we demonstrate the capability of improving predictions of hurricane intensity and structures near landfall by assimilating high-resolution, three-dimensional observations from land-based radars in the landfall regions into a mesoscale NWP model. The landfall of Hurricane Isabel on the east coast of the United States in 2003 is the focus of this study. Observations of Dop-pler radial velocity and reflectivity from five Doppler radars in the landfall region were collected and assimilated into the Navy's Coupled Ocean-Atmosphere Mesoscale Prediction System in a variational data assimilation framework. Four cycles of hourly radar reflectivity data assimilation effectively correct the overprediction of hydrometeor fields by the model, and move the maximum reflectivity regions to the observed locations. Better hurricane structures, including increased maximum wind speed, a tighter inner core, and better organized outer rainbands, are obtained by the radar radial velocity assimilation. Much-improved forecasts of 24-h accumulated precipitation during and after hurricane landfall have also been achieved by the radar data assimilation. The positive results from this study indicate the potential for improving hurricane intensity and structure forecasts by assimilating radar observations into NWP models.
机译:飓风造成的主要损害发生在登陆期间和登陆之后。因此,准确预测飓风在登陆点附近或附近的风和降水对于飓风的准备和减灾至关重要,但它们仍对飓风研究和数值天气预报(NWP)社区构成了挑战。这部分是由于登陆期间飓风强度和结构的快速变化,这与飓风核心区域和外部螺旋雨带的多尺度动力和物理相互作用有关,还与地表条件的突然变化有关。在这项研究中,我们通过将来自登陆区的陆基雷达的高分辨率,三维观测结果吸收到中尺度NWP模型中,证明了改进登陆附近飓风强度和结构的能力。本研究的重点是2003年伊莎贝尔飓风在美国东海岸的登陆。收集了来自登陆区的五台多普勒雷达的多普勒径向速度和反射率的观测值,并将其同化为变分数据同化框架中的海军“海洋-大气中尺度耦合”预测系统。每小时进行四个周期的雷达反射率数据同化可有效纠正模型对水汽流场的过度预测,并将最大反射率区域移至观测位置。通过雷达径向速度同化,可以获得更好的飓风结构,包括提高的最大风速,更紧密的内芯和更好的有组织的外部雨带。雷达数据同化也大大改善了对飓风登陆期间和之后24小时累积降水的预测。这项研究的积极结果表明,通过将雷达观测资料纳入NWP模型,可以改善飓风强度和结构预报。

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