Polar regions receive less intense
solar radiation than the other parts of Earth because the Sun's energy arrives at an
oblique angle, spreading over a larger area, being less concentrated, and also travels a longer distance through Earth's atmosphere in which it may be absorbed, scattered or reflected, which is the same thing that causes winters to be colder than the rest of the year except in tropical regions. The
axial tilt of Earth has the most
effect on climate of the polar regions due to its latitude. However, since the polar regions are the farthest from the
equator, they receive the weakest solar radiation and are therefore generally frigid year round due to Earth's axial tilt of 23.5° not being enough to create a high maximum midday
declination to sufficiently compensate the Sun's rays for the high latitude even in summer, except for relatively brief periods in peripheral areas near the polar circles. The large amount of ice and snow also reflects and weakens of what weak sunlight the polar regions receive further, contributing to the cold. Polar regions are characterized by extremely cold temperatures, heavy
glaciation wherever there is sufficient
precipitation to form permanent
ice, short and still cold summers, and extreme variations in daylight hours, with
twenty-four hours of daylight in summer, and
complete darkness at
mid-winter. ==Circumpolar Arctic region==