The sun is the most useful cause for the heating of the troposphere
The sun is the most useful cause for the heating of the troposphere
no
either conduction or convection
The major contribution in heating the troposphere comes from the sun's radiation. The sun warms the ground by radiation, which in turn warms the air heating the troposphere.
Convection
radiation
The sun heats the Earth, and then longwave radiation heats the troposphere via convection currents.
it is called radiation
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.
Most of the heat in the troposphere is not directly from the sun; rather, it primarily comes from the Earth's surface. The sun heats the land and oceans, which then radiate heat back into the atmosphere, warming the troposphere. Additionally, greenhouse gases trap some of this heat, further contributing to the warming of the lower atmosphere. Thus, while solar radiation is crucial, the heat in the troposphere is a result of both direct sunlight and the Earth's surface processes.
The heating of the air is by radiant heat from the sun.
the sun