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自2016年起,我国大力推进气象业务向"智能化、无缝隙、精准化"发展。2017年宁夏积极推进智能网格预报业务体系建设,在网格预报智能订正、主客观融合订正、格点/站点/落区一体化、灾害天气智能识别等方面开展了一些尝试,取得了一定的成果,目前各项成果均引入到宁夏智能化天气预报业务平台中。其中一项关键技术,是智能网格预报的时空协调一致技术。该项技术在主客观融合订正、格点/站点/落区一体化中发挥了重要作用。本文重点针对这一关键技术的设计思路和实现方法进行介绍、讨论。 相似文献
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Based on the observational hourly precipitation data and the European Centre for Medium-Range Weather Forecasts (ECMWF) Reanalysis 5 (ERA5) products from 2006 to 2020, 22 rainstorm processes in the eastern foot of Helan Mountain are objectively classified by using the hierarchical clustering method, and the circulation characteristics of different patterns are comparatively analyzed in this study. The results show that the occurrences of rainstorm processes in the eastern foot of Helan Mountain are most closely related to three circulation patterns. Patterns I and III mainly occur in July and August, with similar zonal circulations in synoptic backgrounds. Specifically, the South Asia high and the western Pacific subtropical high are stronger and more northward than those in normal years. The frontal systems in westerlies are inactive, while the water vapor from the ocean surface in the south is mainly transported to the rainstorm area by the southerly jet stream at 700 hPa. The dynamic lifting anomalies are relatively weak, the instability of atmospheric stratification is anomalously strong, and thus the localized severe convective rainstorm is more significant. Comparatively, rainstorm processes of pattern I are accompanied by stronger and deeper ascending motions, and the warm-sector rainstorm is more extreme. Pattern III shows a stronger and deeper convective instability, accompanied by larger low-level moisture. Rainstorm processes of pattern II mainly occur in early summer and early autumn, presenting a meridional circulation pattern of high in the east and low in the west in terms of geopotential height. Moreover, the two low-level jets transporting the water vapor northward from the ocean on the east of China encounter with the frontal systems in westerlies, which makes the ascending motion in pattern II anomalously strong and deep. The relatively weak instability of atmospheric stratification causes weak convection and long-lasting precipitation formed by the confluence of cold air and warm air. This study may help improve rainstorm forecasting in arid regions. 相似文献
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