In 2000, Kakade and a colleague conceptualised the Effective Strength Index (ESI), the net relative strength of those two oscillations. The ESI and the ESI-tendency, the evolution of the ESI from winter to spring in the northern hemisphere, can be measured in early May.
If this ESI-tendency is positive, meaning the North Atlantic Oscillation has evolved more strongly than the Southern Oscillation, Kakade will look up the average May temperatures at the sea surface and at 5,572 m above sea level, at specific Arctic locations well defined by their latitude and longitude. Hypothetically, if those May temperatures are higher than normal, they are indicative of a weak Indian summer monsoon, and vice versa.