Rising air for the monsoon is primarily driven by the temperature difference between the land and the surrounding ocean. During the summer months, land surfaces heat up faster than bodies of water, causing the air above the land to rise. This rising air creates a low-pressure system that draws in moist air from the ocean, leading to the development of monsoon rains.
thunderstorms
The winter monsoon, also known as the northeast monsoon in Asia or the trade winds in other regions, brings dry air due to its origin from high-pressure zones over landmasses. As this air flows towards the ocean, it becomes drier as it loses moisture. This phenomenon contributes to the dry season in many areas affected by this type of monsoon.
The storm produced by large rising columns of warm, moist air is typically a thunderstorm. As the warm air rises, it cools and condenses, forming clouds and releasing latent heat, which further fuels the storm. This process can lead to the development of cumulonimbus clouds, heavy rainfall, lightning, and sometimes severe weather phenomena like hail or tornadoes.
Small area storms formed by the strong upward movement of warm, moist air are called storm surges.
Rising and sinking air is called up draft and down draft, respectively.
the land gets heated up due to summer heat because of which hot air rises and mixes with the cold air ans condensation takes place and rain falls
As in other hot countries .
thunderstorms
Thunderstorms are produced by large rising columns of warm moist air. These storms are characterized by intense convective activity, leading to the formation of lightning, thunder, heavy rainfall, and sometimes hail or tornadoes.
thunderstorms
During the summer, seasonal winds called monsoon blow moist air across India from the Indian Ocean.
Mumbai experiences heavy rains during the monsoon due to the presence of the monsoon winds, which bring moist air from the Arabian Sea. When this moist air rises and cools, it condenses to form clouds and eventually leads to heavy rainfall. Topographical factors like the Western Ghats also play a role in enhancing rainfall in the region.
There are two parts to a monsoon; the summer monsoon and the winter monsoon. In the summer monsoon, the land in a tropical location becomes warmer than the ocean. This creates rasing air currents called updrafts. This draws moist air off the ocean. This air then rises and cools, dropping its moisture in the form of heavy rain. In the winter monsoon, dry air is drawn off the land, resulting in little or no rain.
Thunderstorms are produced by large rising columns of warm moist air. This process leads to the formation of cumulonimbus clouds and can result in heavy rainfall, lightning, thunder, and sometimes severe weather such as hail or tornadoes.
The winter monsoon, also known as the northeast monsoon in Asia or the trade winds in other regions, brings dry air due to its origin from high-pressure zones over landmasses. As this air flows towards the ocean, it becomes drier as it loses moisture. This phenomenon contributes to the dry season in many areas affected by this type of monsoon.
The people in India depend on the summer monsoon to bring cold air to the subcontinent
The air pressure is rising.