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# solar constant

solar constant, the average amount of radiant energy received by the earth's atmosphere from the sun; its value is about 2 calories per min incident on each square centimeter of the upper atmosphere. The actual value of the energy varies with several factors; the most important factor is the earth's distance from the sun, which changes because of the earth's elliptical orbit. For computing the value of the solar constant, the astronomical unit, or average earth-sun distance, is used.
The solar luminosity, $L_odot$, is a unit of luminosity (power emitted in the form of photons) conventionally used by astronomers to give the luminosities of stars. It is equal to the current accepted luminosity of the Sun, which is 3.839 × 1026 W, or 3.839 × 1033erg/s. Note that the Sun is a weak variable star and its luminosity therefore fluctuates.

## Calculating with this constant

You can calculate how much solar power hits the Earth by comparing a cross sectional area of the Earth and the total surface area of a sphere with a radius equal to the distance of the earth from the sun.

• The Earth's radius is 3963 miles (6,378 km).
• The Earth's cross sectional area = π×radius2 = 49.3 million square miles (128,000,000 km²).
• The Sun's average distance is about 93 million miles (150,000,000 km).
• The surface area of a sphere = 4×π×radius2 = 1.09×1017 square miles (2.82×1017 km²).
• Power reaching the Earth = P(total) × Area(earth)/Area(sphere) = 1.77×1017 W.
• The power hitting a square meter of area on Earth: (square meter = 1/16092 square miles)
• Power over square meter = P(total)(1/16092)/area(sphere) = 1387 W (the solar constant)