Dominant Large-Scale Atmospheric Circulation Systems for the Extreme Precipitation over the Western Sichuan Basin in Summer 2013

Figure 6

(a) Spatial pattern (the bar) and (b) time series (the bar) of the first mode of the MV-EOF analysis (the solid line denotes the normalized daily precipitation). (c) Composite of 500-hPa normalized geopotential height anomaly. (d) Composite of vertically integrated water vapor transport anomaly (kgm⁻¹s⁻¹) (shading: rainfall > 10 mm).

(a)

(b)

(c)

(d)