All of the molecule$ heat up witch causes it to draw in moisture
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The sun heats the Earth, and then longwave radiation heats the troposphere via convection currents.
All of the molecule$ heat up witch causes it to draw in moisture
All of the molecule$ heat up witch causes it to draw in moisture
As the air in the troposphere heats up from the sun, it becomes less dense and starts to rise. This movement creates vertical air currents and leads to the formation of clouds and precipitation. This process is known as convection.
As the air in the troposphere heats up from the sun, it becomes less dense and expands. This expansion causes the air to rise, creating convection currents. These currents are responsible for many weather phenomena such as wind, clouds, and precipitation.
It usually holds more water because of evaporation and makes the earth very hot.
The major direct source of heat in the troposphere is the sun. Solar radiation warms the Earth's surface, which then heats the air above it through conduction, convection, and radiation. This process creates temperature variations that drive weather patterns and atmospheric circulation.
The air in the Troposphere heats up as it absorbs sunlight, causing it to expand and become less dense. This leads to vertical movement of air, creating convection currents that drive weather patterns and circulation in the atmosphere.
The sun warms the earth's surface, which then heats the air close to the ground through conduction and convection. However, in the troposphere, the air becomes less dense as you move higher, so the sun's energy is spread out over a larger volume of air, making it less effective at heating the air compared to near the surface.
Sources of energy, such as sunlight, reach the troposphere through radiation. Energy from the sun passes through the Earth's atmosphere and is absorbed by the surface, which then heats up and warms the air in the lowest layer of the atmosphere, the troposphere.
In the troposphere, radiation from the sun heats the Earth's surface, which then warms the air in contact with it through conduction. The warm air rises, creating convection currents that transfer heat vertically through the troposphere. This process helps maintain the temperature gradient in the troposphere, with the lower levels warmer than the higher levels.