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Rong-Hua Zhang and Antonio J. Busalacchi

atmospheric response to TIW-induced SST forcing. In this work, we continue to exploit an alternative statistical approach to modeling the TIW-related mesoscale atmospheric variability in the eastern tropical Pacific; a similar approach has been previously taken by Pezzi et al. (2004) who already tested a simple empirical model for TIW–wind feedback that is based on a regression pattern relative to geographically fixed location at 2°N, 140°W (e.g., Hashizume et al. 2001 ). Here, we adopt a combined

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Jianhua Sun and Sixiong Zhao

understand the synoptic background and weather conditions for freezing precipitation events. The previous studies have mainly focused on various regions in North America and Europe, while only very limited number of studies were conducted in China. The investigations in the past with respect to the prediction of freezing precipitation or precipitation types generally fall into the following three categories: (a) Statistical models [e.g., critical thresholds, regression analysis, model output

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