The southwest monsoon (SWM) is the world's most important monsoon system that affects nearly one third of the world population. The SWM maintains a periodicity annually in which more than 80% of the annual precipitation occurs during June-September and represents significant spatial and temporal variation which is dependent upon climatic and topographical features of the Indian subcontinent. The spatial and temporal interannual variability of Indian summer monsoon rainfall (ISMR) leads to large-scale drought and flood, resulting in a major effect on agriculture and the economy of the country (Guhathakurta & Rajeevan, 2006; Naidu et al., 2015; Parthasarathy et al., 1994; Turner & Annamalai, 2012). The strong influence of the Tropical Ocean on the variability of ISMR has been studied and epitomized by the El Nino Southern Oscillation (ENSO) phenomena (Shukla, 1987; Sikka, 1980; Webster & Yang, 1992). ENSO is a phenomenon of coupled ocean-atmosphere used to explain unusual climatic and weather patterns and also disrupt the ecosystem, agriculture, tropical cyclone, drought and flood, and other extreme weather events across the globe. The large-scale ocean-atmosphere climate interaction is linked to the periodic warming in the sea surface temperature (SST) across central and east equatorial Pacific Ocean termed as El Nino. On the other hand, La Nina (a cold event) represents