摘要
本文采用百分位法对观测极端降水的阈值进行定义,根据贝叶斯理论探讨了极端降水的概率预报方法,进行了贝叶斯极端降水模拟概率预报试验和检验。以观测和模式极端降水阈值分别进行的贝叶斯概率预报试验结果表明:以观测极端降水为阈值时,先验概率与后验概率的极端降水空报情况较多,主要降水雨带的概率预报也偏强;而以模式极端降水为阈值时,两者的空报均较少,且对主要雨带也起到了明显的预警作用。对比两种阈值取法下的先验概率和后验概率的极端降水预报,前者的概率预报值较后者的更小。检验结果表明,经过贝叶斯方法修订后的极端降水预报,提高了极端降水产生的正确率,但空报也有所增加。
The threshold of extreme precipitation is defined by the method of percentile method in this paper. Based on Bayesian theory, probabilistic forecasting of extreme precipitation is discussed and we do the Bayesian extreme precipitation experiment and verification. Experiments which are based on observational and modal extreme precipitation threshold show the following conclusions. False prediction of extreme pre- cipitation is proved to be more when the threshold is based on the observational extreme precipitation. The forecast of main rain band is stronger. False prediction is less while the threshold is based on the modal ex- treme precipitation and the early warning to the heavy rain is obvious as well. By contrast, the probabilis- tic forecasting based on the prior probability is smaller. The verifi the extreme precipitation is improved by the Bayesian method, but cat th ion result shows that the accuracy of e false prediction ratio has increased.
出处
《气象》
CSCD
北大核心
2016年第7期799-808,共10页
Meteorological Monthly
基金
中国气象局预报员专项(CMAYBY2014-013)资助
关键词
贝叶斯方法
极端降水
集合预报
北京“7.21”暴雨
Bayesian theory, extreme precipitation, ensemble forecast, "7.21" torrential rain in Beijing