The Sea Surface Temperature (SST) plays a major role in monsoon dynamics, oceanatmosphere
interactions, and cyclone activity in the Bay of Bengal, which is one of
the most climate-sensitive regions of the Indian Ocean. This study shows two
decades (2004-2024) of SST variability and long-term trends in the Bay of Bengal
using multi-satellite datasets from NOAA (OISST v2.1), NASA (MODIS-Aqua), and
Copernicus (CMEMS), calibrating them with in-situ observations from NOAA
moored buoys and ARGO profiling floats. The results indicate a clean basin-wide
warming over the study period, with the highest increases observed during the premonsoon
and monsoon seasons. Seasonal variability is noticeable, with SSTs
ranging from ~25–26 °C in winter to more than 30 0C in April-May. To enhance
confidence in observed patterns, validation with in-situ data confirmed strong
agreement with satellite products. The rising SSTs are correlated with increasing
monsoon variability, which provides favorable conditions for the strong formation
of tropical cyclones. These findings underscore the importance of SST in framing
regional climate and emphasize the need for monitoring of the Bay of Bengal to
build climate resilience.
Keywords: Sea Surface Temperature (SST), Bay of Bengal; Remote Sensing, Climate
Variability, Monsoon, Cyclone Intensification
