Meteorological satellite is a powerful tool because it observes the atmosphere from the space. The remote sensing to the atmosphere frown a satellite has become more and more important in weather prediction since the ...Meteorological satellite is a powerful tool because it observes the atmosphere from the space. The remote sensing to the atmosphere frown a satellite has become more and more important in weather prediction since the meteorological satellites were launched.In United States, Europe and Japan, cloud winds are produced by the successive geostationary satellite images with 30-min interval because they are展开更多
A statistical study of GMS low cloud winds in January,April,July and October,1983 shows that on an average,there exist 223.5 low cloud winds over western North Pacific each synoptic time.The low cloud winds have a diu...A statistical study of GMS low cloud winds in January,April,July and October,1983 shows that on an average,there exist 223.5 low cloud winds over western North Pacific each synoptic time.The low cloud winds have a diurnal change with more low cloud winds at 12 Z than at 00 Z. The wind fields at 850 hPa over western North Pacific,with and without application of low cloud winds, have been analyzed by a successive correction scheme.The results indicate that the flow patterns without low cloud winds are considerably distorted from short of wind data over the oceanic region.On the con- trary,with application of low cloud winds,the flow patterns get much more improved over the oceanic region.展开更多
文摘Meteorological satellite is a powerful tool because it observes the atmosphere from the space. The remote sensing to the atmosphere frown a satellite has become more and more important in weather prediction since the meteorological satellites were launched.In United States, Europe and Japan, cloud winds are produced by the successive geostationary satellite images with 30-min interval because they are
基金supported by the National Natural Science Foundation of China
文摘A statistical study of GMS low cloud winds in January,April,July and October,1983 shows that on an average,there exist 223.5 low cloud winds over western North Pacific each synoptic time.The low cloud winds have a diurnal change with more low cloud winds at 12 Z than at 00 Z. The wind fields at 850 hPa over western North Pacific,with and without application of low cloud winds, have been analyzed by a successive correction scheme.The results indicate that the flow patterns without low cloud winds are considerably distorted from short of wind data over the oceanic region.On the con- trary,with application of low cloud winds,the flow patterns get much more improved over the oceanic region.
