摘要
利用青藏高原及邻近地区(70.~105.E、20.~40°N)2012年1~12月的资料,采用平均误差和均方根误差对EC模式和T213模式数值预报产品的500 hPa高度场进行检验,初步给出量化误差值,分析了2种模式在藏北高原的可预报性.结果发现,EC模式24、48、72h预报场在藏北高原的预报能力较强,T213模式相对于EC模式预报能力较弱,同时利用10次天气过程进行了误差检验及3d滑动误差订正,取得了较好的误差订正效果.
Abstract Using the methods of the mean error and the root - mean - square error, and data from Tibetan Plateau and its adjacent regions (70° -105°E, 20° -40°N) from January to December, 2012, the 500- hPa height contours provided by ECMWF (European Centre for Medium- Range Weather Forecasts) and by the T213 global model from the National Meteorological Center was assessed, and the quantization error to ana- lyses the applicability of these two models to the northern Tibetan Plateau was calculated. The results showed that the ECMWF 24 h, 48 h and 72 h forecast fields have a stronger forecasting capacity on the northern Tibetan Plateau while the T213 has comparatively a weaker forecasting capac- ity. At the same time, with ten weather processes, error check and three - day error correction was carried out with good error correction per- formance.
出处
《安徽农业科学》
CAS
2013年第17期7620-7623,7675,共5页
Journal of Anhui Agricultural Sciences
关键词
数值预报产品
可预报性
检验
藏北高原
Numeral forecast products
Forecasting capacity
Detection
Northern Tibet Plateau