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The North Pole is in the Arctic Ocean, and thus its temperature extremes are buffered by the water.The result is that the South Pole is consistently colder during the southern winter than the North Pole during the northern winter.The low angle of Sun during the winter months means that incoming rays of solar radiation are spread over a larger area of the Earth's surface, so the light received is more indirect and of lower intensity.Between this effect and the shorter daylight hours, the axial tilt of the Earth accounts for most of the seasonal variation in climate in both hemispheres.
This is because the Northern Hemisphere has more land than the Southern, and land warms more readily than sea.
In some parts of the world, some other "seasons" capture the timing of important ecological events such as hurricane season, tornado season, and wildfire season. 1This diagram shows how the tilt of Earth's axis aligns with incoming sunlight around the winter solstice of the Northern Hemisphere. the Earth's rotation on its axis), the North Pole will be dark, and the South Pole will be illuminated; see also arctic winter.
In addition to the density of incident light, the dissipation of light in the atmosphere is greater when it falls at a shallow angle. Regardless of the time of year, the northern and southern hemispheres always experience opposite seasons.
Seasonal weather fluctuations (changes) also depend on factors such as proximity to oceans or other large bodies of water, currents in those oceans, El Niño/ENSO and other oceanic cycles, and prevailing winds.
In the temperate and polar regions, seasons are marked by changes in the amount of sunlight, which in turn often causes cycles of dormancy in plants and hibernation in animals.
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The seasonal cycle in the polar and temperate zones of one hemisphere is opposite to that of the other.