Improving Polarimetric Radar-Based Drop Size Distribution Retrieval and Rain Estimation Using a Deep Neural Network

被引:2
|
作者
Ho, Junho [1 ,2 ]
Zhang, Guifu [1 ,2 ]
Bukovcic, Petar [3 ]
Parsons, David B. [1 ]
Xu, Feng [1 ]
Gao, Jidong [4 ]
Carlin, Jacob T. [3 ]
Snyder, Jeffrey C. [4 ]
机构
[1] Univ Oklahoma, Sch Meteorol, Norman, OK 73072 USA
[2] Univ Oklahoma, Adv Radar Res Ctr, Norman, OK 73071 USA
[3] Univ Oklahoma, Cooperat Inst Severe & High Impact Weather Res & O, Norman, OK USA
[4] NOAA OAR Natl Severe Storms Lab, Norman, OK USA
基金
美国国家科学基金会; 美国海洋和大气管理局;
关键词
Rainfall; Drop size distribution; Radars/Radar observations; Deep learning; Neural networks; Regression; PART I; MICROPHYSICS PARAMETERIZATION; DIFFERENTIAL REFLECTIVITY; WEATHER; CLOUD; DISDROMETER; CALIBRATION; MODEL;
D O I
10.1175/JHM-D-22-0166.1
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Raindrop size distributions (DSD) and rain rate have been estimated from polarimetric radar data using different approaches with the accuracy depending on the errors both in the radar measurements and the estimation meth-ods. Herein, a deep neural network (DNN) technique was utilized to improve the estimation of the DSD and rain rate by mitigating these errors. The performance of this approach was evaluated using measurements from a two-dimensional video disdrometer (2DVD) at the Kessler Atmospheric and Ecological Field Station in Oklahoma as ground truth with the re-sults compared against conventional estimation methods for the period 2006-17. Physical parameters (mass-/volume-weighted diameter and liquid water content), rain rate, and polarimetric radar variables (including radar reflectivity and differential reflec-tivity) were obtained from the DSD data. Three methods-physics-based inversion, empirical formula, and DNN-were ap-plied to two different temporal domains (instantaneous and rain-event average) with three diverse error assumptions (fitting, measurement, and model errors). The DSD retrievals and rain estimates from 18 cases were evaluated by calculating the bias and root-mean-squared error (RMSE). DNN produced the best performance for most cases, with up to a 5% reduction in RMSE when model errors existed. DSD and rain estimated from a nearby polarimetric radar using the empirical and DNN methods were well correlated with the disdrometer observations; the rain-rate estimate bias of the DNN was significantly re-duced (3.3% in DNN vs 50.1% in empirical). These results suggest that DNN has advantages over the physics-based and empiri-cal methods in retrieving rain microphysics from radar observations.
引用
收藏
页码:2057 / 2073
页数:17
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