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

<div>Monthly location of the Western Pacific Subtropical High (indicated by 5865 gpm contour) for (a) climatology (averaged for the period of 1950–2017), (b) cool PDO in developing summers, (c) warm PDO in developing summers, (d) cool PDO in decaying summers, and (e) warm PDO in decaying summers. Red, green, and blue lines represent June, July, and August, respectively.</div>

Advances in Meteorology

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Figure 3

Figure 3: CP El Niño and PDO Variability Affect Summer Precipitation over East China 