CP El Niño and PDO Variability Affect Summer Precipitation over East China

Figure 11

Monthly averaged OLR anomalies over the western equatorial Pacific (10°S–40°N, 110°–140°E) in cool ((a) and (b)) and warm ((c) and (d)) PDO phase from developing to decaying CP El Niño years. (a) Developing period, western Pacific OLR. (b) Decaying period, western Pacific OLR. (c) Developing period, western Pacific OLR. (d) Decaying period, western Pacific OLR.

(a)

(b)

(c)

(d)