A Machine Learning Approach to Model Over-Ocean Tropical Cyclone Precipitation

被引:2
|
作者
Lockwood, Joseph W. [1 ,2 ]
Loridan, Thomas [2 ]
Lin, Ning [3 ]
Oppenheimer, Michael [1 ,4 ,5 ]
Hannah, Nic [2 ]
机构
[1] Princeton Univ, Dept Geosci, Princeton, NJ 08544 USA
[2] Reask, London, England
[3] Princeton Univ, Civil & Environm Engn, Princeton, NJ USA
[4] Princeton Univ, Princeton Sch Publ & Int Affairs, Princeton, NJ USA
[5] High Meadows Environm Inst, Princeton, NJ USA
关键词
Precipitation; Tropical cyclones; Machine learning; Principal components analysis; VERTICAL WIND SHEAR; EXTRATROPICAL TRANSITION; HURRICANE HARVEY; RAINFALL; EVOLUTION; MOTION; RISK;
D O I
10.1175/JHM-D-23-0065.1
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Extreme rainfall found in tropical cyclones (TCs) is a risk for human life and property in many low-to mid -latitude regions. Probabilistic modeling of TC rainfall in risk assessment and forecasting can be computationally expensive, and existing models are largely unable to model key rainfall asymmetries such as rainbands and extratropical transition. Here, a machine learning-based framework is developed to model overwater TC rainfall for the North Atlantic basin. First, a catalog of high-resolution TC precipitation simulations for 26 historical events is assembled for the North Atlantic basin using the Weather Research and Forecasting (WRF) Model. The simulated spatial distribution of rainfall for these historical events are then decomposed via principal component analysis (PCA), and quantile regression forest (QRF) mod-els are trained to predict the conditional distributions of the first five principal component (PC) weights. Conditional distri-butions of rain-rate levels are estimated separately using historical satellite data and a QRF model. With these models, probabilistic predictions of rainfall maps can be made given a set of storm characteristics and local environmental condi-tions. The model is able to capture storm total rainfall compared to satellite observations with a correlation coefficient of 0.96 and r2 value of 0.93. Additionally, the model shows good accuracy in modeling hourly total rainfall compared to satel-lite observations. Rain-rate maps predicted by the model are also compared to historical satellite observations and to the WRF simulations during cross validation, and the spatial distribution of estimates captures rainfall variability consistent with TC rainbands, wavenumber asymmetries, and possibly extratropical transition.
引用
收藏
页码:207 / 221
页数:15
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