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使用下投式探空仪的飓风成像辐射计(HIRAD)风速反演与验证

Hurricane Imaging Radiometer (HIRAD) Wind Speed Retrievals and Validation Using Dropsondes.

作者信息

Cecil Daniel J, Biswas Sayak K

机构信息

NASA Marshall Space Flight Center, Huntsville, AL.

Universities Space Research Association, Huntsville, AL.

出版信息

J Atmos Ocean Technol. 2017 Aug;34(8):1837-1851. doi: 10.1175/JTECH-D-17-0003.1. Epub 2017 Aug 22.

Abstract

Surface wind speed retrievals have been generated and evaluated using Hurricane Imaging Radiometer (HIRAD) measurements from flights over Hurricane Joaquin, Hurricane Patricia, Hurricane Marty, and the remnants of Tropical Storm Erika, all in 2015. Procedures are described here for producing maps of brightness temperature, which are subsequently used for retrievals of surface wind speed and rain rate across a 50 km wide swath for each flight leg. An iterative retrieval approach has been developed to take advantage of HIRAD's measurement characteristics. Validation of the wind speed retrievals has been conducted, using 636 dropsondes released from the same WB-57 high altitude aircraft carrying HIRAD during the Tropical Cyclone Intensity (TCI) experiment. The HIRAD wind speed retrievals exhibit very small bias relative to the dropsondes, for winds tropical storm strength (17.5 m s) or greater. HIRAD has reduced sensitivity to winds weaker than tropical storm strength, and a small positive bias (2 m s) there. Two flights with predominantly weak winds according to the dropsondes have abnormally large errors from HIRAD, and large positive biases. From the other flights, root mean square differences between HIRAD and the dropsonde winds are 4.1 m s (33%) for winds below tropical storm strength, 5.6 m s (25%) for tropical storm strength winds, and 6.3 m s (16%) for hurricane strength winds. Mean absolute differences for those categories are 3.2 m s (25%), 4.3 m s (19%), and 4.8 m s (12%), with bias near zero for tropical storm and hurricane strength winds.

摘要

利用2015年对飓风华金、飓风帕特里夏、飓风马蒂以及热带风暴埃丽卡残余部分进行飞行探测时飓风成像辐射计(HIRAD)的测量数据,生成并评估了地面风速反演结果。本文描述了生成亮温图的程序,这些亮温图随后用于反演每次飞行航段约50公里宽扫描带的地面风速和降雨率。已开发出一种迭代反演方法,以利用HIRAD的测量特性。利用热带气旋强度(TCI)实验期间从搭载HIRAD的同一架WB - 57高空飞机上释放的636个下投探空仪,对风速反演结果进行了验证。对于热带风暴强度(17.5米/秒)及以上的风,HIRAD风速反演结果相对于下投探空仪显示出非常小的偏差。HIRAD对弱于热带风暴强度的风的敏感性降低,且存在小的正偏差(约2米/秒)。根据下投探空仪数据,有两次主要为弱风的飞行探测中,HIRAD的误差异常大且正偏差大。在其他飞行探测中,对于弱于热带风暴强度的风,HIRAD与下投探空仪风速之间的均方根差异为4.1米/秒(33%);对于热带风暴强度的风,差异为5.6米/秒(25%);对于飓风强度的风,差异为6.3米/秒(16%)。这些类别对应的平均绝对差异分别为3.

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