Abstract Pacific Meridional Mode (PMM) has been found to be significantly correlated with tropical cyclone (TC) genesis in the western North Pacific (WNP), while the seasonality in their relationship remains unknown. Here we found that their relationship experiences remarkable seasonality, with a significant positive correlation in January–April and August–December but an insignificant relationship in May–July. This seasonality stems from the diverse responses of large‐scale conditions to the different magnitude of the PMM‐related sea surface temperature (SST) warming that is dependent on the strength of trade wind in the three seasons. In January–July, strong trade wind facilitates great PMM SST warming that stimulates large‐scale ascending motion in the eastern WNP but compensated descending motion in the western WNP, favoring TC genesis in January–April because its main genesis region is in the eastern WNP. However, the main genesis region extends to the whole WNP in May–July, the inconsistent large‐scale condition anomalies across the western and eastern WNP thus lead to the insignificant relationship in May–July. In August–December, the PMM‐related SST warming and the associated ascending motion fade away due to the much‐weakened trade wind, and the favorable large‐scale ascending motion over the whole WNP is linked to the PMM‐related SST cooling induced descending motion through a modification of the Walker circulation. The results highlight the season‐dependent mechanism of PMM influencing TC genesis and have some insights for improving seasonal forecasting.
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