A Case Study of Mass Transport during the East-West Oscillation of the Asian Summer Monsoon Anticyclone

Figure 7

A pressure-longitude cross section of vertical velocity along 20°N on (a) Aug 3, (b) Aug 5, (c) Aug 7, (d) Aug 9, (e) Aug 10, and (f) Aug 14, 2016. Gray shading regions indicate upward. Regions within black contours are strong upward motion regions (contour level is −10 Pa/s).

(a) Vertical velocity [m/s] at 20°N on Aug 3, 2016

(b) Vertical velocity [m/s] at 20°N on Aug 5, 2016

(c) Vertical velocity [m/s] at 20°N on Aug 7, 2016

(d) Vertical velocity [m/s] at 20°N on Aug 9, 2016

(e) Vertical velocity [m/s] at 20°N on Aug 10, 2016

(f) Vertical velocity [m/s] at 20°N on Aug 14, 2016