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Reconstruction of Hurricane Katrina's wind fields for storm surge and wave hindcasting

机译:重建卡特里娜飓风的风场,以进行风暴潮和波后预报

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As the most costly US natural disaster in history, Hurricane Katrina fostered the IPET forensic study to better understand the event. All available observations from several hundred space-, land-, sea-, and aircraft-based measurement platforms were gathered and processed to a common framework for height, exposure, and averaging time, to produce a series of wind field snapshots at 3 h intervals to depict the wind structure of Katrina when in the Gulf of Mexico. The stepped-frequency microwave radiometer was calibrated against GPS sondes to establish the upper range of the instrument and then used to determine the wind field in the storm's core region in concert with airborne Doppler radar winds adjusted to the surface from near the top of the PBL (500 m). The SFMR data were used to develop a method to estimate surface winds from 3 km level reconnaissance aircraft observations, taking into consideration the observed azimuthal variation of the reduction factor. The "SFMR method" was used to adjust reconnaissance flight-level measurements to the surface in the core region when SFMR and Doppler winds were not available. A variety of coastal and inland mesonet data were employed, including portable towers deployed by Texas Tech University, University of Louisiana at Monroe, and the Florida Coastal Monitoring Program, as well as fixed mesonet stations from Louisiana State Universities Marine Consortium, University of Southern Mississippi, and Agricultural Networks from Louisiana, Mississippi, and Alabama, and the Coastal Estuarine Network of Alabama and Mississippi. Also included were land- (WSR-88D VAD and GBVTD, ASOS, Metar, LLWAS, HANDAR), space- (QuikScat, GOES cloud drift winds, WindSat), and marine- (GPS sondes, Buoys, C-MAN, ships) platforms. The wind fields serve as an analysis of record and were used to provide forcing for wave and storm surge models to produce hindcasts of water levels in the vicinity of flood control structures.
机译:作为美国历史上最昂贵的自然灾害,卡特里娜飓风促进了IPET法医研究,以更好地了解这一事件。收集了来自数百个基于空间,陆地,海洋和飞机的测量平台的所有可用观测值,并将其处理到一个有关高度,暴露和平均时间的通用框架中,以每3小时间隔生成一系列风场快照描绘了在墨西哥湾时卡特里娜飓风的结构。使用GPS探测仪对步进式微波辐射计进行校准,以建立仪器的上限范围,然后与从PBL顶部附近调整到地面的机载多普勒雷达风一起用于确定风暴核心区域的风场(500 m)。 SFMR数据用于开发一种方法,该方法可从3 km高度的侦察机观测值中估计地表风,同时考虑到观测到的减小因子的方位角变化。当SFMR和多普勒风不可用时,使用“ SFMR方法”将侦察飞行高度测量值调整到核心区域的地面。使用了各种沿海和内陆的介子站数据,包括德克萨斯理工大学,路易斯安那大学门罗分校和佛罗里达海岸监测计划部署的便携式塔架,以及路易斯安那州立大学海洋财团,南密西西比大学的固定介子站。 ,以及路易斯安那州,密西西比州和阿拉巴马州的农业网络,以及阿拉巴马州和密西西比州的沿海河口网络。还包括陆地(WSR-88D VAD和GBVTD,ASOS,Metar,LLWAS,HANDAR),太空(QuikScat,GOES云漂移风,WindSat)和海洋(GPS探空仪,浮标,C-MAN,船舶)平台。风场是对记录的分析,并被用来为海浪和风暴潮模型提供强迫,以在防洪结构附近产生水位的后预报。

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