Research Article
Observational and Simulative Study of a Local Severe Precipitation Event Caused by a Cold Vortex over Northeast China
Figure 16
Vertical cross section of the differences in the meridional velocity (shaded, m s−1) and vertical velocity (isolines, m s−1) between 23:00 and 22:00 27 July 2010 along 125°E, and the 1 h precipitation of 22:00-23:00 (red histogram, mm) (the dashed rectangle indicates an area of strong convergence between the southerly and northerly winds).