1) The seasons are caused by variations in the intensity and duration of solar radiation received at different latitudes throughout the year. The tilt of the Earth's axis of rotation relative to its orbit around the sun causes the seasons. 2) During the winter solstice in the Northern Hemisphere, days get shorter the farther north you travel. 3) The angle of the noon sun and the intensity of solar radiation received at the outer edge of the atmosphere are directly related, with higher sun angles resulting in greater intensities.