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首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >Improved track forecasting of a typhoon reaching landfall from four-dimensional variational data assimilation of AMSU-A retrieved data
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Improved track forecasting of a typhoon reaching landfall from four-dimensional variational data assimilation of AMSU-A retrieved data

机译:改进跟踪预报的台风从四维变分数据登陆简称amsu - a检索数据的同化

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摘要

In this study, an attempt to improve typhoon forecasts is made by incorporating three-dimensional Advanced Microwave Sounding Unit-A (AMSU-A) retrieved wind and temperature and the central sea level pressure of cyclones from typhoon reports or bogus surface low data into initial conditions, on the basis of the Fifth-Generation National Center for Atmospheric Research/Pennsylvania State University Mesoscale Model (MM5) four-dimensional variational data assimilation (4DVar) system with a full-physics adjoint model. All the above-mentioned data are found to be useful for improvement of typhoon forecasts in this mesoscale data assimilation experiment. The comparison tests showed the following results: (1) The assimilation of the satellite-retrieved data was found to have a positive impact on the typhoon track forecast, but the landing position error is ~150 km. (2) The assimilation of both the satellite-retrieved data and moving information of the typhoon center dramatically improved the track forecast and captured the recurvature and landfall. The mean track error during the 72-hour forecast is 69 km. The predicted typhoon intensity, however, is much weaker than that from observations. (3) The assimilation of both the satellite-retrieved data and the bogus surface low data improved the intensity and track forecasts more significantly than the assimilation of only bogus surface low data (bogus data assimilation) did. The mean errors during the 72-hour forecast are 2.6 hPa for the minimum sea level pressure and 87 km for track position. However, the forecasted landing time is ~6 hours earlier than the observed one.
机译:在这项研究中,为了提高台风预测是由合并三维高级微波探测业务——一个检索(简称amsu - a)的风和温度和中央海平面气压的气旋从台风报告或虚假的表面低数据为初始条件,的基础上第五代国家中心的大气研究中尺度/宾夕法尼亚州立大学四维变分模型(MM5)数据full-physics同化(4 dvar)系统伴随模型。发现有用的改进的台风预测在这个中尺度数据同化实验。以下结果:(1)的同化satellite-retrieved数据被发现有一个对台风路径预报,产生积极的影响但着陆位置误差~ 150公里。的同化satellite-retrieved数据和信息的台风中心移动大大提高了预测和跟踪捕获折回原来方向和登陆。跟踪误差在72 - 69公里小时预测。然而,预测台风强度是多少不如,从观察。同化的satellite-retrieved数据和虚假的表面低数据提高了强度和跟踪预测更重要同化的只有虚假的表面低数据(虚假的数据同化)。错误在72 - 2.6 hPa小时预测最低海平面气压和87公里跟踪位置。时间是比观察到的早~ 6小时。

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