主办单位:中国气象局沈阳大气环境研究所
国际刊号:ISSN 1673-503X
国内刊号:CN 21-1531/P

气象与环境学报 ›› 2013, Vol. 29 ›› Issue (2): 12-18.doi:

• 论文 • 上一篇    下一篇

MOS方法在短时要素预报中的应用与检验

李文娟1 郦敏杰2   

  1. 1.浙江省气象台,浙江 杭州310017;2.杭州市气象局,浙江 杭州310051
  • 出版日期:2013-04-30 发布日期:2013-04-30

Application and verification of MOS statistical method for forecasting of short time meteorological elements

LI Wen-juan1 LI Min-jie2   

  1. 1.Zhejiang Meteorological Observatory, Hangzhou 310017, China; 2. Hangzhou Meteorological Service, Hangzhou 310051, China
  • Online:2013-04-30 Published:2013-04-30

摘要: 通过对MM5数值预报产品的释用,将MOS统计方法应用到短时要素预报中,综合利用MM5数值预报产品、自动站实况数据和雷达数据等资料,建立降水和温度的4 h预报模型;降水作为不连续变量,将其通过建立降水可能函数的方法转化为连续变量,利用统计预报方法,可以达到定量预报的目的。通过对4140个时次的样本进行检验。结果表明:MOS预报结果较MM5直接输出结果整体有所改进,当数值模式误差较大时,统计方法显示出一定的优势;降水预报检验结果显示,TS评分为65%,预报正确率PC为91%。降水明显的样本(3 h雨量>5 mm)平均误差在8 mm以内,弱降水样本(3 h雨量<3 mm)平均误差在1 mm以内,预报方程对非雨日样本的整体预报效果较好,优于MM5模式预报,预报正确率高达98%,但对流性降水仍是预报难点;对于温度预报,20—08时段误差较小、平均在1.0℃以内,而11—17时、误差平均在1.5℃左右,但经过误差的季节订正,可以控制在1.0℃左右。

关键词: MOS统计方法, 短时要素预报, 降水可能函数, TS评分, MOS统计方法, 短时要素预报, 降水可能函数, TS评分

Abstract:  Through the interpretation of MM5 numerical prediction products, the MOS statistical method was applied to forecast short time meteorological elements. A forecast model of precipitation and temperature with 4 hours interval was established in terms of MM5 numerical prediction products, the observational data from automatic weather stations and the radar data. Precipitation was a discontinuous variable, but it could be translated into a continuous variable by establishing a possibility function of precipitation. Thus, quantitative forecasting could be realized. 4140 samples were tested in this paper. The results show that MOS method is better than the MM5 method, especially for the cases when errors with the MM5 method are higher. According to the test of precipitation prediction, TS score is 65 % and the accuracy reaches 91%. The average error is less than 8mm for heavy rain samples (three hours accumulated rainfall > 5 mm), while it is 1 mm or less for weak precipitation samples (three hours accumulated rainfall < 1 mm). The MOS method has the higher accuracy with 98% for the prediction the non-rain day, and it is better than the MM5 prediction. However, the convective precipitation is still hard to forecast. For the temperature model, the error is less than 1.0 ℃ from 20:00 to 08:00, while it is 1.5 ℃ from 11:00 to 17:00.  The error can be controlled about 1.0 ℃ after season corrections.

Key words: MOS statistical method, Short-term Elements forecasting, Possibility function of precipitation, TS score, MOS statistical method, Forecasting of short term meteorological elements, Possibility function of precipitation, TS score