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

<div>Differences of the winter (November-March) mean surface wind between the warm PDO phases and cool PDO years from developing (a) to decaying (b) CP El Niño years.</div>

Advances in Meteorology

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Figure 12

Figure 12: CP El Niño and PDO Variability Affect Summer Precipitation over East China 