Yang Junho, Jun Mikyoung, Schumacher Courtney, Saravanan R
Department of Statistics, Texas A&M University, College Station, Texas.
Department of Atmospheric Sciences, Texas A&M University, College Station, Texas.
J Clim. 2019 Jun;32(11):3409-3427. doi: 10.1175/jcli-d-18-0527.1. Epub 2019 May 17.
This study explores the feasibility of predicting subdaily variations and the climatological spatial patterns of rain in the tropical Pacific from atmospheric profiles using a set of generalized linear models: logistic regression for rain occurrence and gamma regression for rain amount. The prediction is separated into different rain types from TRMM satellite radar observations (stratiform, deep convective, and shallow convective) and CAM5 simulations (large-scale and convective). Environmental variables from MERRA-2 and CAM5 are used as predictors for TRMM and CAM5 rainfall, respectively. The statistical models are trained using environmental fields at 0000 UTC and rainfall from 0000 to 0600 UTC during 2003. The results are used to predict 2004 rain occurrence and rate for MERRA-2/TRMM and CAM5 separately. The first EOF profile of humidity and the second EOF profile of temperature contribute most to the prediction for both statistical models in each case. The logistic regression generally performs well for all rain types, but does better in the east Pacific compared to the west Pacific. The gamma regression produces reasonable geographical rain amount distributions but rain rate probability distributions are not predicted as well, suggesting the need for a different, higher-order model to predict rain rates. The results of this study suggest that statistical models applied to TRMM radar observations and MERRA-2 environmental parameters can predict the spatial patterns and amplitudes of tropical rainfall in the time-averaged sense. Comparing the observationally trained models to models that are trained using CAM5 simulations points to possible deficiencies in the convection parameterization used in CAM5.
用逻辑回归预测降雨发生情况,用伽马回归预测降雨量。预测分为基于热带降雨测量任务(TRMM)卫星雷达观测的不同降雨类型(层状、深对流和浅对流)以及气候模式比较计划第5版(CAM5)模拟的不同降雨类型(大尺度和对流)。分别将现代时代感测资料同化系统第2版(MERRA-2)和CAM5的环境变量用作TRMM和CAM5降雨的预测因子。统计模型利用协调世界时0000时的环境场以及2003年协调世界时0000至0600时的降雨进行训练。结果分别用于预测2004年MERRA-2/TRMM和CAM5的降雨发生情况和降雨率。在每种情况下,湿度的第一经验正交函数(EOF)廓线和温度的第二EOF廓线对两个统计模型的预测贡献最大。逻辑回归对所有降雨类型总体表现良好,但在东太平洋比西太平洋表现更好。伽马回归产生了合理的地理降雨量分布,但降雨率概率分布的预测效果不佳,这表明需要一个不同的高阶模型来预测降雨率。本研究结果表明,应用于TRMM雷达观测和MERRA-2环境参数的统计模型能够在时间平均意义上预测热带降雨的空间模式和幅度。将基于观测训练的模型与使用CAM5模拟训练的模型进行比较,指出了CAM5中对流参数化可能存在的不足。