A small part of the heating is directly from the sun. But a lot of heating near the surface is done through conduction by the land that has been warmed by the sun. The atmosphere can also be heated in several other ways; by radiation, global warming, the greenhouse effect, convection and conduction.
The process you are referring to is called evaporation. Evaporation occurs when the sun's energy heats up water on the Earth's surface, causing it to turn into water vapor and rise into the atmosphere.
Energy from the geosphere is primarily transferred to the atmosphere through processes like radiation and conduction. Solar radiation heats the Earth's surface, which in turn heats the air above it. This warmed air rises due to convection, transferring energy to the atmosphere.
Solar radiation—The sun emits energy in the form of electromagnetic radiation, which heats the Earth's atmosphere. Infrared radiation—The Earth's surface absorbs solar radiation and emits heat energy in the form of infrared radiation, which warms the atmosphere. Convection—The warmed air near the Earth's surface rises, carrying heat energy higher into the atmosphere and contributing to the overall warming.
The sun heats the atmosphere. Solar radiation largely passes through the atmosphere and warms the surface of the earth. The earth then radiates heat up into the lower levels of the atmosphere where greenhouse gases warm. The warmed greenhouse gases then continue to radiate heat in all directions warming the atmosphere and again the earth's surface.
it gets absorbed by the ground
no it's infared radition
Earth's atmosphere gets energy primarily from the sun. Solar radiation heats the atmosphere, creating temperature gradients and driving weather patterns. Some energy is also exchanged between the atmosphere and the Earth's surface through processes like conduction, convection, and evaporation.
The process you are referring to is called evaporation. Evaporation occurs when the sun's energy heats up water on the Earth's surface, causing it to turn into water vapor and rise into the atmosphere.
The primary source of energy that heats the atmosphere is the Sun. Solar radiation warms the Earth's surface, which in turn heats the lower atmosphere through conduction and convection. Additionally, the atmosphere also retains some heat from the Earth's surface.
The energy in the earth's atmosphere primarily originates from the Sun. The Sun heats the earth and the water, heating the atmosphere.
The Sun's energy heats the atmosphere.
Heat!!
Heat!!
Energy from the geosphere is primarily transferred to the atmosphere through processes like radiation and conduction. Solar radiation heats the Earth's surface, which in turn heats the air above it. This warmed air rises due to convection, transferring energy to the atmosphere.
Solar radiation—The sun emits energy in the form of electromagnetic radiation, which heats the Earth's atmosphere. Infrared radiation—The Earth's surface absorbs solar radiation and emits heat energy in the form of infrared radiation, which warms the atmosphere. Convection—The warmed air near the Earth's surface rises, carrying heat energy higher into the atmosphere and contributing to the overall warming.
the altitude
The sun heats the atmosphere. Solar radiation largely passes through the atmosphere and warms the surface of the earth. The earth then radiates heat up into the lower levels of the atmosphere where greenhouse gases warm. The warmed greenhouse gases then continue to radiate heat in all directions warming the atmosphere and again the earth's surface.