模式:

ICON(ICOsahedral Nonhydrostatic general circulation model) from the German Weather Service

更新:
4 times per day, from 08:00, 14:00, 20:00, and 00:00 UTC
格林尼治平时:
12:00 UTC = 20:00 北京时间
Resolution:
0.125° x 0.125°
参量:
Tmin 2m:
地面以上2米处的最低温度
描述:
这幅图显示由ANV-模式算出的6到12点和12到18点UTC的最低温度。 尽管模式算出的2米-温度同实测值常常不一致,但是只要满足下列条件:
1. 有850百帕温度资料;
2. 有天气报;
3. 有经验的预报员,
报好Tmin 2m 是完全可能的。

ICON:
ICON The ICON dynamical core is a development initiated by the Max Planck Institute for Meteorology (MPI-M) and the Opens external link in current windowGermany Weather Service (DWD). This dynamical core is designed to better tap the potential of new generations of high performance computing, to better represent fluid conservation properties that are increasingly important for modelling the Earth system, to provide a more consistent basis for coupling the atmosphere and ocean and for representing subgrid-scale heterogeneity over land, and to allow regionalization and limited area implementations.
NWP:
Numerical weather prediction uses current weather conditions as input into mathematical models of the atmosphere to predict the weather. Although the first efforts to accomplish this were done in the 1920s, it wasn't until the advent of the computer and computer simulation that it was feasible to do in real-time. Manipulating the huge datasets and performing the complex calculations necessary to do this on a resolution fine enough to make the results useful requires the use of some of the most powerful supercomputers in the world. A number of forecast models, both global and regional in scale, are run to help create forecasts for nations worldwide. Use of model ensemble forecasts helps to define the forecast uncertainty and extend weather forecasting farther into the future than would otherwise be possible.

Wikipedia, Numerical weather prediction, http://zh.wikipedia.org/wiki/數值天氣預報(as of Feb. 9, 2010, 20:50 UTC).