Seasons

A year is divided by changes in weather, ecology and hours of daylight. These changes are called seasons. Our seasons are the result of the A visual representation of the seasonsyearly revolution of the earth around the sun and the tilt of the earth. The earth's axis is an imaginary line that runs through the middle of the earth from the North Pole to the South Pole. The axis of the earth is tilted about 23½ degrees. The tilt of the earth remains the same as the earth follows its yearly path around the sun. This path is known as an orbit.

In June, the Northern Hemisphere is tilted toward the sun, so the people in the Northern Hemisphere have longer and warmer days. The days are shorter and colder in the Southern Hemisphere in June, because the earth is tilted away from the sun. The days start getting shorter in the Northern Hemisphere and longer in the Southern Hemisphere after June 21. Daytime lasts exactly as long as nighttime on the first day of autumn (September 21) and the first day of spring (March 21). The first day of winter in the Northern Hemisphere, on December 21, is the shortest day of the year in the Northern Hemisphere and the longest day of the year in the Southern Hemisphere.

Seasonal changes are more pronounced as you move further away from the equator. The area that is 23½ degrees north and south of the equator is known as the tropics. The tropics receive direct rays from the sun all year long, so tropical regions have less seasonal variation than the temperate and polar regions that cover the rest of the earth. Many plants and animals in the regions beyond the tropics have adapted to the changing of the seasons. This is why many plants become dormant in the winter months, and why some animals follow a seasonal journey known as a migration.

The days get longer in summer and shorter in winter as you move from the equator. It's generally dark on a summer night in Florida by 8:30 p.m., but in Vermont, there will still be some light at 10:00 p.m. The situation is reversed in the winter, where the sun will go down in Vermont by 3:45 p.m. while it remains light in Florida until 5:15 p.m. Northern Alaska is called the "Land of the Midnight Sun" because it never gets dark during the summer months. That part of the earth is facing the sun all day and all night. Antarctica never sees daylight during those months. The situation is reversed in December and January when northern Alaska never sees the sun while it continues to light the sky at night in Antarctica.

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To cite this page (MLA):

Dowling, Mike. "Seasons at mrdowling.com." www.mrdowling.com. Updated March 25, 2013 . Web. Date of Access. <http://www.mrdowling.com/601-seasons.html>