To fully understand the "why," compare the two rain-bearing systems:
Several geographical and atmospheric factors ensure that the rain arrives only after the summer heat has fully prepared the stage: why maximum rainfall in india occurs after the summer season
The lag between summer and peak rainfall is a matter of physics and geography. The summer season acts as the engine that powers the monsoon machine; it creates the vacuum, generates the heat, and sets the stage. The rainfall is the consequence of that setup. Therefore, the skies remain largely clear during the hottest days, and the heavens open up with maximum ferocity only after the summer heat has done its work of pulling the winds inland. To fully understand the "why," compare the two
The maximum rainfall in India occurs during the months of July and August, which is after the summer season. This delay is due to the time it takes for the southwest monsoon to establish itself over the country and for the weather systems to mature. The monsoon trough, which is a belt of low-pressure systems that forms over the Indian subcontinent, also plays a significant role in the distribution of rainfall. As the monsoon trough shifts northwards during July and August, it brings the rain-bearing clouds to the northern parts of the country, resulting in heavy rainfall. Therefore, the skies remain largely clear during the
During summer, the vast Indian landmass, including the Thar Desert and the Tibetan Plateau , heats up significantly faster than the surrounding oceans. This intense heat causes the air above the land to rise, creating a massive low-pressure zone .