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首页> 外文期刊>Journal of hydrometeorology >Value of a Dual-Polarized Gap-Filling Radar in Support of Southern California Post-Fire Debris-Flow Warnings
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Value of a Dual-Polarized Gap-Filling Radar in Support of Southern California Post-Fire Debris-Flow Warnings

机译:支持南加州大火后泥石流预警的双极化间隙填充雷达的价值

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Aportable truck-mounted C-band Doppler weather radar was deployed to observe rainfall over the Station Fire burn area near Los Angeles, California, during the winter of 2009/10 to assist with debris-flow warning decisions. The deployments were a component of a joint NOAA–U.S. Geological Survey (USGS) research effort to improve definition of the rainfall conditions that trigger debris flows from steep topography within recent wildfire burn areas. A procedure was implemented to blend various dual-polarized estimators of precipitation (for radar observations taken below the freezing level) using threshold values for differential reflectivity and specific differential phase shift that improves the accuracy of the rainfall estimates over a specific burn area sited with terrestrial tipping-bucket rain gauges. The portable radar outperformed local Weather Surveillance Radar-1988 Doppler (WSR-88D) National Weather Service network radars in detecting rainfall capable of initiating post-fire runoff-generated debris flows. The network radars underestimated hourly precipitation totals by about 50%. Consistent with intensity–duration threshold curves determined from past debris-flow events in burned areas in Southern California, the portable radar-derived rainfall rates exceeded the empirical thresholds over a wider range of storm durations with a higher spatial resolution than local National Weather Service operational radars. Moreover, the truck-mounted C-band radar dual-polarimetric-derived estimates of rainfall intensity provided a better guide to the expected severity of debris-flow events, based on criteria derived from previous events using rain gauge data, than traditional radar-derived rainfall approaches using reflectivity–rainfall relationships for either the portable or operational network WSR-88D radars. Part of the reason for the improvement was due to siting the radar closer to the burn zone than the WSR-88Ds, but use of the dual-polarimetric variables improved the rainfall estimation by ;12% over the use of traditional Z–R relationships.
机译:在2009/10年度冬季,部署了便携式卡车安装的C波段多普勒天气雷达,以观测加利福尼亚州洛杉矶附近的Station Fire燃烧区的降雨,以协助做出泥石流预警决策。这些部署是美国国家海洋和大气管理局(NOAA)与美国联合的组成部分。地质调查局(USGS)的研究工作旨在改善降雨条件的定义,这些条件会触发最近的野火燃烧区域内陡峭地形的泥石流。实施了一种程序,使用差分反射率和特定差分相移阈值来混合各种双极化的降水估计量(用于在冻结水平以下进行雷达观测),从而提高了地面特定燃烧区域的降雨估计的准确性翻斗式雨量计。便携式雷达在检测能够引发火后径流产生的泥石流的降雨方面,胜过了当地的气象监视雷达1988多普勒(WSR-88D)国家气象服务网络雷达。网络雷达低估了每小时的降水总量约50%。与根据南加州燃烧地区过去泥石流事件确定的强度-持续时间阈值曲线一致,便携式雷达得出的降雨率在更广泛的风暴持续时间范围内超过了经验阈值,且空间分辨率高于当地国家气象局的运行雷达。此外,与以往的雷达测算方法相比,基于先前雨量计数据得出的标准,车载式C波段雷达双极化法得出的降雨强度估算值可以更好地指导泥石流事件的预期严重性。对于WSR-88D便携式或可操作网络雷达,采用反射率与降雨关系的降雨方法。改进的部分原因是由于雷达的位置比WSR-88D更靠近燃烧区域,但与传统Z–R关系相比,双极化变量的使用使降雨估算提高了12%。

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