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I think you are referring to the Annual cycle of the seasons.

This occurs due to the orientation of the axis of the Earth's rotation with respect to the ecliptic, the plane in which the Earth (and to a reasonably similar degree) the other planets orbit the sun.

Since the axis of the Earth's rotation points almost exactly in the same direction in space throughout time, (This is an approximation though. See an article on precession for more on that), and since the axis is inclined at an angle of about 23 degrees to the normal to the ecliptic, the Earth will at diametrically opposite points in it's orbit be pointed 23 degrees towards the sun and 23 degrees away from the sun.

This has the effect of making the sun trace out a smaller path in the sky during winter. The points where it breaks the horizon when setting and rising are closer together than during summer and it doesn't reach as high in the sky. This is due to the shape of the Earth. If we lived on a rotating cylinder we would notice the intensity of the light would be lower in winter and summer than during autumn and spring, and also that the sun didn't reach as high but the day length would remain unchanged from one season to the next. Essentially the larger diameter of lower more equitorial latitudes occludes part of the suns path across the sky when the Earth's rotational axis is turned away from the sun.

Hope this helped.

Try this from wikipedia too:

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Q: Why do the days get longer and shorter?
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