The Okhotsk-Japan Circulation Pattern and the Heavy Rainfall in Beijing in 2012 Summer

Figure 6

The time evolution of daily 500 hPa geopotential height deviations (contour interval: 10 gpm) along A–F (Figure 4) (a) and surface pressure (solid line, unit: hPa) and 850 hPa water vapor flux divergence (dashed line, unit: kg/(s hPa m²)) in Beijing (b) from July 10 to 31, 2012.

(a)

(b)