Solar Energy And The Atmosphere Worksheet Answers

Explain how you calculated the amount of energy generated per month.

Solar energy and the atmosphere worksheet answers.

Start studying science test worksheet energy in earth s atmosphere. Most of the short wave energy produced by the sun passes easily through the atmosphere and heats the surface of the earth. Some of this energy is bounced back out by the earth as heat which warms the troposphere. The three types are.

5 0 kwh m2 day x 30 days month x 200 m2 x 0 12 3600 kwh month stop and think. Of the solar energy that reaches the outer atmosphere uv wavelengths have the greatest energy. The earth receives 174 petawatts of incoming solar. Quiz worksheet goals practice questions will discuss.

Solar energy hits the earth s atmosphere and heats it. For worksheet answer explanations refer to the solar power energy estimation worksheet answers to find the latitude of your location which is needed in order to determine the tilt angle of a solar module visit the noaa solar calculator web page or use any internet browser to search for the latitude of your location latitude is measured in. 6 6 kwh m2 day x 30 days month x 200 m2 x 0 12 4752 kwh month portland. Renewable energy living lab.

4 0 kwh m2 day x 30 days month x 200 m2 x 0 12 2880 kwh month san antonio. These incoming 51 units consist of shorter wavelength solar radiation mostly in the visible region of the electromagnetic spectrum which is absorbed by land water and vegetation. Solar energy and climate change the earth s climate is changing because of an ever increasing amount of greenhouse gas ghg emissions in the atmosphere. The earth s surface then returns long wave energy into the.

Only about 7 of solar radiation is in the uv wavelengths. 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. Topics of questions will be the origin of solar radiation types of energy transfer gases in the atmosphere and the warmth of earth.

At the mesopause the temperature begins to increase with altitude and this trend continues in the thermosphere. The mesosphere does not absorb solar heat so the temperature decreases with altitude. The atmosphere and clouds absorb 19 units of this incoming solar radiation leaving 51 units of solar radiation that is absorbed at earth s surface. Although solving climate change will likely require a combination of targeted technologies solar technologies have a huge role to play in curbing emissions.