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Objective Tropical Cyclone Center Tracking Using Single-Doppler Radar

机译:单多普勒雷达客观热带气旋中心跟踪

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This study presents an extension of the ground-based velocity track display (GBVTD)-simplex tropical cyclone (TC) circulation center-finding algorithm to further improve the accuracy and consistency of TC center estimates from single-Doppler radar data. The improved center-finding method determines a TC track that ensures spatial and temporal continuities of four primary characteristics: the radius of maximum wind, the maximum axisymmetric tangential wind, and the latitude and longitude of the TC circulation center. A statistical analysis improves the consistency of the TC centers over time and makes it possible to automate the GBVTD-simplex algorithm for tracking of landfalling TCs. The characteristics and performance of this objective statistical center-finding method are evaluated using datasets from Hurricane Danny (1997) and Bret (1999) over 5-h periods during which both storms were simultaneously observed by two coastal Weather Surveillance Radar-1988 Doppler (WSR-88D) units. Independent single-Doppler and dual-Doppler centers are determined and used to assess the absolute accuracy of the algorithm. Reductions of 50% and 10% in the average distance between independent center estimates are found for Danny and Bret, respectively, over the original GBVTD-simplex method. The average center uncertainties are estimated to be less than 2 km, yielding estimated errors of less than 5% in the retrieved radius of maximum wind and wavenumber-0 axisymmetric tangential wind, and similar to 30% error in the wavenumber-1 asymmetric tangential wind. The objective statistical center-finding method can be run on a time scale comparable to that of a WSR-88D volume scan, thus making it a viable tool for both research and operational use.
机译:这项研究提出了地面速度跟踪显示(GBVTD)-简单热带气旋(TC)循环中心查找算法的扩展,以进一步提高从单多普勒雷达数据获得的TC中心估计的准确性和一致性。改进的中心查找方法确定了TC轨迹,该轨迹可确保四个主要特征的空间和时间连续性:最大风的半径,最大轴对称切向风以及TC循环中心的纬度和经度。进行统计分析可提高TC中心随时间推移的一致性,并使GBVTD-simplex算法自动化以跟踪降落TC成为可能。使用来自飓风丹尼(1997)和布雷(1999)的数据集在5小时内通过两个沿海天气监视雷达1988多普勒(WSR)同时观测到两次暴风雨的数据集,评估了该客观统计中心发现方法的特征和性能。 -88D)单位。确定独立的单多普勒和双多普勒中心,并将其用于评估算法的绝对精度。与最初的GBVTD-simplex方法相比,Danny和Bret的独立中心估计之间的平均距离分别减少了50%和10%。平均中心不确定性估计小于2 km,在最大风和波数为0的轴对称切向风的取回半径中产生的估计误差小于5%,与波数为1的不对称切向风的误差近似为30% 。客观的统计中心发现方法可以在与WSR-88D体积扫描相当的时间范围内运行,从而使其成为可行的研究和运营工具。

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