Fig. 2: Statistics of post-monsoon season Bay of Bengal cyclones during El Niño (La Niña) and positive IOD (negative IOD) years (1979–2020). | npj Climate and Atmospheric Science

Fig. 2: Statistics of post-monsoon season Bay of Bengal cyclones during El Niño (La Niña) and positive IOD (negative IOD) years (1979–2020).

From: ENSO influence on Bay of Bengal cyclogenesis confined to low latitudes

Fig. 2

Number of cyclonic storms (CS) and severe cyclonic storms (SCS) formed over the low latitudes (LLC, originated between 5°N–10°N) and high latitudes (HLC, originated in a latitude >10°N) during El Niño, La Niña, positive IOD (PIOD) and negative IOD (NIOD) years.

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