The south Asian summer monsoon, also known as the Indian Summer Monsoon (ISM) is the strongest monsoon system in the world. Although the ISM arrives regularly every summer, seasonal accumulated rainfall (i.e., ISMR) varies and that has a significant impact on the country's food production (Gadgil & Kumar, 2006), freshwater availability for drinking, and industrial uses. However, the prediction of the ISMR in one season advance has remained subcritical (Kumar et al., 2005; Rajeevan et al., 2010). Even though the tropical climate is considered more predictable than its extratropical counterpart (Charney & Shukla, 1981), the ISM is an exception due to strong influences by the chaotic nature of subseasonal variability (Goswami et al., 2006; Webster et al., 1998). Contributions of the subseasonal rainfall to the seasonal anomaly are primarily considered as noise due to their origin from higher frequency chaotic component of the monsoon system, that leads to low potential predictability of the ISMR (