preprint https://arxiv.org/abs/2012.04384 A review of the ocean-atmosphere interactions during tropical cyclones in the north Indian Ocean Vineet Kumar Singh1,2 and M.K. Roxy1* 1 Indian Institute of Tropical Meteorology, Ministry of Earth Sciences, Pune, India 2 Department of Atmospheric and Space Sciences, Savitribai Phule Pune University, Pune, India Earth Science Reviews, submitted on 9 November 2020, Revised on 31 July 2021 *Corresponding author address: Roxy Mathew Koll, Indian Institute of Tropical Meteorology, Pune 411008, India. E-mail:
[email protected] 1 preprint https://arxiv.org/abs/2012.04384 Abstract The north Indian Ocean accounts for 6% of the global tropical cyclones annually. Despite the small fraction of cyclones, some of the most devastating cyclones have formed in this basin, causing extensive damage to the life and property in the north Indian Ocean rim countries. In this review article, we highlight the advancement in research in terms of ocean-atmosphere interaction during cyclones in the north Indian Ocean and identify the gap areas where our understanding is still lacking. There is a two-way ocean-atmosphere interaction during cyclones in the north Indian Ocean. High sea surface temperatures (SSTs) of magnitude 28–29°C and above provide favorable conditions for the genesis and evolution of cyclones in the Arabian Sea and the Bay of Bengal. On the other hand, cyclones induce cold and salty wakes with SST cooling of 2–3°C during the pre- monsoon season and 0.5–1°C during the post-monsoon season. This varying response in the two seasons in the Bay of Bengal is due to the difference in the ocean haline stratification, whereas, in the Arabian Sea it is due to the difference in cyclone wind power input and ocean thermal stratification.