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Kingtse C. Mo, Lindsey N. Long, and Jae-Kyung E. Schemm

compensated by overly strong negative anomalies in April–June (AMJ). This indicates that, in order to simulate realistic FOC for drought or persistent wet spells, the model only needs to capture the mean responses of P during ENSO. All models have an ENSO signal in the tropics, but not all models capture the P response to ENSO. This suggests that to have the ENSO mode alone is not enough for a model to capture the FOC for drought and persistent wet spells. The model also needs to capture the tropical

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