“…Even if atmospheric conditions are promising, TC will not develop if the SST is low (Lin et al, 2008) and difficult to occur in SSTs < 26 ºC (Emanuel, 2003). In the ocean region bordering the Indonesian seas, especially in the southeastern part of the tropical Indian Ocean, several TCs have occurred, such as Anggrek (October 31 -November 4, 2010), Bakung (December 10 -13, 2014), Cempaka (November 25 -27, 2017), Dahlia (November 27 -December 2, 2017), (Paterson, 2012;Gutro, 2014;Samodra et al, 2020;Yang et 2020;Aditya et al, 2021) and Seroja ; Latos et al, 2022). TC events can cause critical oceanic phenomena in the form of cooling SSTs (Hazelworth, 1968;Stramma, Cornillon and Price, 1986;Leipper, 1967;Lin et al, 2013).…”