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

The zonal-vertical cross sections of energy divergence flux and its components in Eq. (6) along 31.2° N at valley 1 time (shaded, kg·m−1·s−2, (a), (c), (e), (g), and (i)) and peak 1 time (contour, kg·m−1·s−2, superposed with vertical motion, m·s−1, (b), (d), (f), (h), (j)). (a) and (b) −υ · E; (c) and (d) −υ · p; (e) and (f) −E · υ; (g) and (h) −p · υ; (i) and (j) − · [υ(E + p)]. (k) The three-dimensional divergence (shaded, 10−4 s−1), temperature perturbation (contour, K), and wind vector (m·s−1). (l) The same as that in panel (j), except at 10 min-later time.