Image of local energy anomaly during a heavy rainfall event
Yang Shuai1, Zuo Qunjie1, †, Gao Shouting1, 2
       

The vertical distributions of total energy perturbation from background separation along the strong convection centers (31.2° N herein), representing the total energy anomaly (contour, kg·m−1·s−2). The vertical motion is superposed with shaded (m·s−1) (a) at valley 1 time; (b) at peak 1 time; (c) at valley 2 time; (d) at peak 2 time.