Research Article
Characteristic Features of the Evolution of a Meiyu Frontal Rainstorm with Doppler Radar Data Assimilation
Figure 11
Temporal evolution of vertically integrated water vapor flux (unit: g·kg−1·m·s−1) from surface to 850 hPa averaged over (113°–118°E, 28°−30°N). X-axis indicates the forecasting time 0–24 h from 0000 UTC 4–0000 UTC 5 July 2014.