首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >Seasonal tropical cyclone precipitation in Texas: A statistical modeling approach based on a 60 year climatology
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Seasonal tropical cyclone precipitation in Texas: A statistical modeling approach based on a 60 year climatology

机译:德克萨斯州的季节性热带气旋降水:一种基于60年气候学的统计建模方法

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摘要

Sixty years of tropical cyclone precipitation (TCP) in Texas has been analyzed because of its importance in extreme hydrologic events and the hydrologic budget. We developed multiple linear regression models to provide seasonal forecasts for annual TCP, TCP's contribution (percentage) to total precipitation, and the number of TCP days in Texas. The regression models are based on three or fewer predictors with model fits ranging from 0.18 to 0.43 (R~2) and cross-validation accuracy of 0.05-0.36 (R~2). La Ni?a exhibits the most important control on TCP in Texas. It is the major driver in our models and acts to reduce the vertical shear in the Caribbean and the tropical Atlantic, thereby generating more precipitating storms in Texas. Lower maximum potential velocity, the theoretical maximum wind speed that storms can attain, in the Gulf of Mexico, and low-level vorticity in the Atlantic hurricane main development region increased the modeled R~2 by 20% or more. Both variables have negative coefficients in the TCP models. Lower maximum potential velocity and vorticity are associated with tropical cyclones with lower maximum wind speed and slower translation speed. Such weak TCs produce the majority of TCP and extreme TCP events in Texas. The quartiles of the TCs with strongest maximum wind speed and fastest translation speed are not associated with the largest mean daily precipitation based on observations in Texas. We have also shown that sea level pressure in the Gulf of Mexico, sea surface temperature in the Caribbean, and the North Atlantic Oscillation are potentially important predictors of seasonal TCP in Texas.
机译:由于其在极端水文事件和水文预算中的重要性,因此已经分析了德克萨斯州六十年的热带气旋降水(TCP)。我们开发了多个线性回归模型,以提供年度TCP,TCP对总降水量的贡献(百分比)以及德克萨斯州TCP天数的季节性预测。回归模型基于三个或更少的预测变量,模型拟合范围为0.18至0.43(R〜2),交叉验证准确性为0.05-0.36(R〜2)。 La Ni?a在德克萨斯州展示了对TCP的最重要控制。它是我们模型的主要驱动力,其作用是减少加勒比海和热带大西洋的垂直切变,从而在德克萨斯州引发更多的暴风雨。在墨西哥湾,较低的最大潜在速度,风暴可以达到的理论最大风速以及在大西洋飓风主要开发区域的低涡度使模拟的R〜2增大了20%或更多。在TCP模型中,两个变量的系数均为负。较低的最大潜在速度和涡度与较低的最大风速和较慢的平移速度的热带气旋有关。如此弱的TC产生了德克萨斯州的大多数TCP和极端TCP事件。根据德克萨斯州的观测,最大风速和最快平移速度最大的四分位数与平均日降水量最大无关。我们还表明,墨西哥湾的海平面压力,加勒比海的海面温度和北大西洋涛动可能是德克萨斯州季节性TCP的重要预测因子。

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