The Arabian sea severe cyclone “Agni” in November formed very close to the equator near latitude 1.5N. Cyclogenesis over the north Indian Ocean at such low latitudes has not occurred in the past. The coexistence of cyclonic disturbances over the Arabian sea and the Bay of Bengal as occurred in June 2004 is also not common. This had however helped the progress of the southwest monsoon across the country during the onset phase.
This was the first North Indian season that featured the naming of storms, though only two storms received names.