Cyclonic or frontal rainfall is caused by the convergence of warm and cold air masses. The warm, moist air is forced to rise over the cold, denser air, leading to condensation and precipitation.
Explanation:
Heat wave conditions in northern India during summer are caused by intense solar radiation, hot dry winds (loo) from the Thar Desert, and clear skies that allow maximum heating of the land surface.
Explanation:
Tropical cyclones intensify over warm ocean waters (typically above 26°C) because the warm water provides the energy (latent heat) needed to fuel the storm. Cold water, wind shear, and landfall weaken the cyclone.
Explanation:
The Western Ghats receive high rainfall during the southwest monsoon due to orographic lifting. Moisture-laden monsoon winds rise over the mountains, cool, condense, and release heavy rainfall on the windward side.
No comments yet. Be the first to start the discussion!