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well the sun obviously gives a constant amount of light. the real factor for the amount of daylight is the earth its orbit around the sun and how it is tilted on its axis. everybody automatically assumes the earths orbit around the sun is a circle but it is more of a oval (egg) shape so the earth will be closer to the sun twice a year (the equinox) plus the earth tilts slightly on its axis as it travels along its orbit. on one equinox the top hemisphere is closer to the sun so you get warmer weather and longer days and on the other the Southern Hemisphere is closer giving them there summer.

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