摘要
Since L. F. Richardson introduced the concept of numerical weather prediction in 1922, it has become an important part of meteorological services. The operational nurnerical weather prediction of large-scale atmospheric circulation systems has a 30-year history, but precipitation forecasting and nowcasting of meso-scale severe weather remain in its experimental stage, and the advance of their numerical predictions is slow. Theoretical studies indicate that the predictability time lhnit of the convective storm-scale system has
基金
Project supported by the Laboratory of Numerical Modelling for Atmospheric Sciences
Geophysical Fluid Dynamics (LASG), Academia Sinica