Solar Energy In The Atmosphere

Of the solar energy that reaches the outer atmosphere uv wavelengths have the greatest energy.

Solar energy in the atmosphere.

Solar energy systems power plants do not produce air pollution water pollution or greenhouse gases. The second highest energy is also mostly stopped in the atmosphere. Photosynthesis captures approximately 3 000 ej per year in biomass. Total solar irradiance tsi is a measure of the solar powerover all wavelengths per unit area incident on the earth s upper atmosphere.

Energy released from the sun is emitted as shortwave light and ultraviolet energy. At night when the sun sets and the atmosphere has cooled the materials release their heat back into the atmosphere. The three types are. The lowest energy travels through the atmosphere to the ground.

The highest energy ultraviolet does not reach the planet s surface at all. It is measured perpendicularto the incoming sunlight. Only about 7 of solar radiation is in the uv wavelengths. When it reaches the earth some is reflected back to space by clouds some is absorbed by the atmosphere and some is absorbed at the earth s surface.

The approximate average value cited 1 3608 0 0005 kw m which is 81 65 kj m per minute is equivalent to approximately 1 951 calories per minute per. Sunlight at the top of earth s atmosphere is composed by total energy of about 50 infrared light 40 visible light and 10 ultraviolet light. The atmosphere in particular filters out over 70 of solar ultraviolet especially at the shorter wavelengths. The earth atmosphere energy balance is the balance between incoming energy from the sun and outgoing energy from the earth.

Using solar energy can have a positive indirect effect on the environment when solar energy replaces or reduces the use of other energy sources that have larger effects on the environment. Homes and other buildings use passive solar energy to distribute heat efficiently and inexpensively. Passive solar energy techniques take advantage of this natural heating and cooling process. The total solar energy absorbed by earth s atmosphere oceans and land masses is approximately 3 850 000 exajoules ej per year.

In 2002 this was more energy in one hour than the world used in one year. Solar irradiance is measured by satellites above earth s atmosphere and is then adjusted using the inverse square law to infer the magnitude of solar irradiance at one astronomical unit au to evaluate the solar constant. The solar constantis a conventional measure of mean tsi at a distance of one astronomical unit au.