Solar Energy In The Atmosphere

Energy released from the sun is emitted as shortwave light and ultraviolet energy.

Solar energy in the atmosphere.

The second highest energy is also mostly stopped in the atmosphere. The total solar energy absorbed by earth s atmosphere oceans and land masses is approximately 3 850 000 exajoules ej per year. The lowest energy travels through the atmosphere to the ground. 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.

Only about 7 of solar radiation is in the uv wavelengths. The earth atmosphere energy balance is the balance between incoming energy from the sun and outgoing energy from the earth. Homes and other buildings use passive solar energy to distribute heat efficiently and inexpensively. Photosynthesis captures approximately 3 000 ej per year in biomass.

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. Passive solar energy techniques take advantage of this natural heating and cooling process. The three types are. Temperature differences in the atmosphere are a result of the way solar energy is absorbed as it moves through the atmosphere.

It is measured perpendicularto the incoming sunlight. The highest energy ultraviolet does not reach the planet s surface at all. The thermosphere or the upper atmosphere is the height region above 85 km while the region between the tropopause and the mesopause is the middle atmosphere stratosphere and mesosphere where absorption of solar uv radiation generates the temperature maximum near 45 km altitude and causes the ozone layer. The atmosphere in particular filters out over 70 of solar ultraviolet especially at the shorter wavelengths.

Solar energy systems power plants do not produce air pollution water pollution or greenhouse gases. In 2002 this was more energy in one hour than the world used in one year. Total solar irradiance tsi is a measure of the solar powerover all wavelengths per unit area incident on the earth s upper atmosphere. The solar constantis a conventional measure of mean tsi at a distance of one astronomical unit au.

The transfer of heat energy within the atmosphere hydrosphere and the earth s surface and interior occurs as a result of radiation convection and conduction. 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. Of the solar energy that reaches the outer atmosphere uv wavelengths have the greatest energy.