LAND IN SOLAR ENERGY SOLAR RADIATION EARTH
The energy received from the sun, cross the Earth's atmosphere heats the water vapor in the atmosphere some areas more than others, causing changes in the density of the gases and thus causing imbalances atmospheric circulation. This energy causes the temperature at the surface and the effect of the atmosphere is enhanced by and mitigate the greenhouse effect the temperature difference between day and night and between the pole and Ecuador.
Most of the energy used by living organisms from the sun, the plants absorb it directly and perform photosynthesis , herbivores indirectly absorb a small amount of this energy by eating plants, and carnivores indirectly absorb a smaller amount eating herbivores.
Most energy sources used by humans are derived indirectly from the sun, as the sun can throughout their radiation energy released to be tapped as humans. Preserved fossil fuels makes solar energy captured by photosynthesis millions of years, hydropower potential energy uses water that condensed in height after being evaporated by the heat of the sun, etc.
albedo albedo The is the ratio, expressed as a percentage of radiation that any surface reflects on the radiation incident on it. The bright areas have higher albedo values \u200b\u200bfor dark and bright than maths. The average albedo of the Earth is 30-32% of the radiation from the sun .
is a measure of the tendency of a surface to reflect radiation incident. In
astronomy offers an indirect means to ascertain the nature of a star by comparing the albedo with known materials. The highest recorded so far in the solar system corresponds to the satellite Enceladus Saturn of , and the lowest some carbonaceous asteroids and the Martian satellites Phobos and Deimos. Http://feedjit.com/join/
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