期刊
WEATHER AND FORECASTING
卷 36, 期 3, 页码 915-928出版社
AMER METEOROLOGICAL SOC
DOI: 10.1175/WAF-D-20-0210.1
关键词
Mesoscale forecasting; Numerical weather prediction; forecasting; Operational forecasting; Short-range prediction; Convective parameterization
资金
- National Key Research and Development Program of China [2017YFC150190X, 2016YFE0109700]
- National Science Foundation of China [41975133]
The study suggests that choosing the proper convection parameterization can improve the precipitation forecast skill in the 9-km operational system at the Shanghai Meteorological Service, with the impacts varying depending on geographical regions and weather regimes.
The quantitative precipitation forecast in the 9-km operational modeling system (without the use of a convection parameterization scheme) at the Shanghai Meteorological Service (SMS) usually suffers from excessive precipitation at the grid scale and less-structured precipitation patterns. Two scale-aware convection parameterizations were tested in the operational system to mitigate these deficiencies. Their impacts on the warm-season precipitation forecast over China were analyzed in case studies and two-month retrospective forecasts. The results from case studies show that the importance of convection parameterization depends on geographical regions and weather regimes. Considering a proper magnitude of parameterized convection can produce more realistic precipitation distribution and reduce excessive gridscale precipitation in southern China. In northeast and southwest China, however, the convection parameterization plays an insignificant role in precipitation forecast because of strong synoptic-scale forcing. A statistical evaluation of the two-month retrospective forecasts indicates that the forecast skill for precipitation in the 9-km operational system is improved by choosing proper convection parameterization. This study suggests that improvement in contemporary convection parameterizations is needed for their usage for various meteorological conditions and reasonable partitioning between parameterized and resolved convection.
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