La Nina is a climate pattern characterized by the cooling of the sea surface temperature in the central and eastern tropical Pacific Ocean.
This phenomenon has a significant impact on global weather patterns, including the Indian monsoon.
Strengthening the monsoon: During a La Nina year, the trade winds are stronger than usual, which pushes warmer water towards Asia and strengthens the atmospheric circulation that drives the Indian monsoon. This results in above-average rainfall for most of the Indian subcontinent.
Weakening effect: Conversely, an El Nino event (the warming of the same waters) typically weakens the Indian monsoon, often leading to drought-like conditions.