The Sun is the primary source of solar radiation, which is a form of electromagnetic energy emitted by the Sun.

Solar radiation encompasses a wide range of wavelengths, including visible light, ultraviolet radiation, and infrared radiation.

Solar radiation is more intense at lower latitudes because the Sun's rays strike the Earth's surface at a more direct angle.

Solar radiation heats the Earth's surface, which then transfers heat to the air through conduction, convection, and radiation.

Solar radiation heats the Earth's surface unevenly, leading to the formation of pressure gradients and wind patterns that influence the distribution of rainfall.

The intensity of solar radiation reaching the Earth's surface is influenced by latitude, time of day, and season.

Solar radiation provides energy for photosynthesis, stimulates seed germination, and promotes plant growth.

Western India, particularly the Thar Desert region, receives the highest amount of solar radiation due to its low latitude and clear skies.

Solar radiation heats the Indian Ocean, which leads to the formation of low-pressure areas that attract moisture-laden winds from the Arabian Sea and the Bay of Bengal, resulting in the monsoon.

Areas with low solar radiation, such as the Thar Desert, receive less rainfall and have sparse vegetation.

Elevation does not directly influence the amount of solar radiation reaching a particular location on Earth.

Solar radiation heats the Earth's atmosphere primarily through radiation, as it is a form of electromagnetic energy.

The Thar Desert, located in Western India, experiences the longest duration of sunshine throughout the year due to its clear skies and low cloud cover.

Solar radiation heats the Earth's surface, causing water to evaporate. This water vapor rises and cools, causing it to condense into clouds.

Atmospheric pressure does not directly affect the intensity of solar radiation reaching the Earth's surface.