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

<div>Zonal distributions of the composite winter (November-March) mean tropical surface zonal wind anomalies in developing (a) and decaying (b) CP El Niño years during the warm PDO (red line) and cool PDO (blue line) phases.</div>

Advances in Meteorology

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Figure 13

Figure 13: CP El Niño and PDO Variability Affect Summer Precipitation over East China 