Context
IMD in a press briefing has forecast that the rains in June-September will be 6% more than these months, an annual average of 87 cm.
India to Get Above Normal Rain this Monsoon Season 2024
- The forecasts also indicate that “above-normal” rain was likely over most parts of the country except northwest, east and northeast India.
- The models indicate a 30% chance of monsoon rains being over 10%, categorized as ‘excess’.
- Usually the chances of excess rain in any given year is only a 17%
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- Factors:
- Emerging La Nina: The El Nino is expected to fade away by June and progress to La Nina (a converse cooling effect in the Central Pacific region that is usually linked to surplus rainfall by the second half of the monsoon ie. August and September).
- A positive Indian Ocean Dipole (A cooler than normal Indian Ocean in the east as compared to the west) though currently ‘neutral’, it is expected to turn positive by August.
- It will help bring rain to several States in southern India.
- Below normal snow cover in the Northern Hemisphere and Eurasia: The snow cover level in Eurasia and Indian monsoon shares an inverse relationship
- Approach used by IMD to forecast monsoon:
- Statistical Approach: To draw upon IMDs vast historical database of over 150 years to correlate certain global meteorological parameters such as ocean temperatures and snow cover in Europe etc. to the performance of the monsoon.
- Dynamic Approach: It is to simulate the weather across the globe on a particular day, and to extrapolate this weather into any future day or time period desired.
Indian Monsoon

- Indian Monsoon is a seasonal change in the direction of the prevailing, or strongest, winds of a region.
- India gets southwest monsoon winds in the summers (formation of an intense low-pressure system over the Tibetan Plateau) and northeast monsoons during the winters (due to the high-pressure cells that are formed over the Siberian and Tibetan plateaus.)
- Factors affecting the onset of monsoon
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- Intense low-pressure formation over the Tibetan Plateau due to intense heating of landmass during summers
- The permanent high-pressure cell in the South of the Indian Ocean near madagascar
- Subtropical jet stream
- African Easterly jet (Tropical easterly jet)
- low-pressure systems (or monsoon depressions), presence of ITCZ (InterTropical Convergence Zone)
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Also Read: Changing Rainfall Patterns In India’s Sub-Districts
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