(a) The differential heating and cooling of land and water creates low pressure on the landmass of India while the seas around experience comparatively high pressure.
(b) The shift of the position of Inter Tropical Convergence Zone (ITCZ) in summer, over the Ganga plain (this is the equatorial trough normally positioned about 5°N of the equator - also known as the monsoon trough during the monsoon season).
(c) The presence of the high-pressure area, east of Madagascar, approximately at 20°S over the Indian ocean. The intensity and position of this high-pressure area affects the Indian Monsoon.
(d) The Tibetan plateau gets intensely heated during summer, which results in strong vertical air currents and the formation of high pressure over the plateau at about 9 km above sea level.
(e) The movement of the westerly jet stream to the north of the Himalayas and the presence of the tropical easterly jet stream over the Indian peninsula during summer.
Latosols (predominantly yellow latosols)
A tropical rainforest climate typically has a lot of rain throughout the year, with high humidity and abundant vegetation. Other climates with high levels of rainfall include temperate rainforest climates and monsoon climates.
Common characteristics used to classify climates include temperature, precipitation, humidity, wind patterns, and seasonal variations. These factors help determine the type of climate a region falls under, such as tropical, arid, temperate, or polar climates.
Monsoon climates provide ample rainfall for agriculture, ensuring sufficient water for crops. The seasonal variation in rainfall helps regulate temperature and prevent extreme weather conditions. Additionally, monsoon winds bring moisture from oceans, supporting biodiversity and ecosystems.
India's climate is characterized by its diversity, with tropical wet, tropical dry, subtropical humid, and montane climates found across the country. The country experiences three main seasons - summer, monsoon, and winter - with variations in temperature and precipitation. The southwest monsoon brings the majority of India's rainfall between June and September.
Latosols (predominantly yellow latosols)
Monsoon climates typically consist of monthly mean temperatures of 18 degrees Celsius, and tend to have less variances in temperature. These climates also have have wet seasons and pronounced dry seasons.
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A sudden heavy rain is called a downpour or a squall and generally occur in monsoon climates which are located near the Equator. Monsoon rains are often violent, strong and sudden.
A sudden heavy rain is called a downpour or a squall and generally occur in monsoon climates which are located near the Equator. Monsoon rains are often violent, strong and sudden.
A tropical rainforest climate typically has a lot of rain throughout the year, with high humidity and abundant vegetation. Other climates with high levels of rainfall include temperate rainforest climates and monsoon climates.
lots of rain heavy winds and big waves
Climate change creates monsoons and cultivation will suffer.
Tropical climates have two seasons, the wet season and the dry season. The monsoon is a seasonal change in wind direction in those types of climates.
Monsoon weather is characterized by heavy rainfall, strong winds, and high humidity. It often brings torrential downpours, thunderstorms, and flooding to the region. Monsoon seasons typically alternate between wet and dry periods in tropical and subtropical climates.
Sub humid tropical climates are characterized by hot, humid summers and mild winters. Sub humid tropical climates get the most rainfall during their summer monsoon months.