模式:

GME (Global weather forecast model) from the German Weather Service

更新:
2 times per day, from 10:00 and 23:00 UTC
格林尼治平时:
12:00 UTC = 20:00 北京时间
Resolution:
0.25° x 0.25°
参量:
RH 600-3000:
地面以上600到3000米之间的平均相对湿度
描述:
这幅图显示地面以上600到3000米之间大气层的平均相对湿度。 虽然这幅图不如925或700百帕等压面相对湿度图那样重要 ,但是它能反映 600米到3000米之间云的形成。

GME:
GME is the first operational weather forecast model which uses an icosahedral-hexagonal grid covering the globe. In comparison to traditional grid structures like latitude-longitude grids the icosahedral-hexagonal grid offers the advantage of a rather small variability of the area of the grid elements. Moreover, the notorious "pole-problem" of the latitude-longitude grid does not exist in the GME grid.
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).