Here's the science of the winter solstice

For many of us on Earth this year, celebrating the first day of winter, astronomically speaking, is more than a yearning for snow-covered landscapes and sips of hot chocolate — It also means we're closer than ever to the end of the year … and the beginning of a new one! 

But the winter solstice is an astronomical marvel in its own right. Today, the Northern Hemisphere experiences the fewest hours of daylight for the year all because of our blue marble's tilt as it treks around the sun. 

Although the solstice gets an entire day of recognition, it happens in an instant: At 10:59 a.m. EST (1559 GMT) on Tuesday (Dec. 21), when the North Pole is at its farthest tilt of 23.5 degrees away from the sun. This position leaves the North Pole beyond the sun's reach, and plunges it into total darkness, according to EarthSky.org.

In the Southern Hemisphere, the sun will shine directly overhead at noon at exactly 23.5 degrees south of the equator, along the imaginary latitude line known as the Tropic of Capricorn, which runs through Australia, Chile, southern Brazil and northern South Africa. This is when when the sun appears to be at its southernmost point in the sky; as such, the Southern Hemisphere has its longest day of the year, and the Northern Hemisphere has its shortest day of the year, on the December solstice, according to EarthSky. 

Related: 6 ancient tributes to the winter solstice

At the moment of the solstice, the sun will also reach its southernmost point in the sky in the Northern Hemisphere. After that moment, the sun will stop moving southward and will begin its trek northward in the sky — hence the name "solstice," which means "sun stands still" in Latin, according to NASA.

After the winter solstice, the days will begin to get longer in the Northern Hemisphere. But that doesn't mean temperatures will increase immediately. Rather, northern midlatitudes will experience the winter chill partly, because they'll get about 9 hours of daylight in the weeks following the solstice, compared with the roughly 15 hours of daily sunlight they get around the summer solstice, Live Science previously reported. In addition, the Northern Hemisphere is tilted away from the sun, making it colder.

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In addition, even as the days get longer, the oceans, which moderate temperatures on land, need a vast amount of energy from the sun to heat up.

Countless cultures have recognized the winter solstice. The most famous is in Stonehenge in England. When the sun sets on the shortest day of the year, the sun's rays align with Stonehenge's central Altar stone and Slaughter stone, which may have had spiritual significance to the people who built the monument, Live Science reported in 2013.

Across the world in Mexico's Yucatan Peninsula, the ancient stonewalled Mayan city of Tulum also has a structure honoring the solstices. When the sun rises on the winter and summer solstices, its rays shine through a small hole at the top of one of the stone buildings, which creates a starburst effect.

Editor's note: This article was originally published Dec. 21, 2017. It was updated on Dec. 21, 2021.

Original article on Live Science.


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Originally posted on: https://www.livescience.com/57280-winter-solstice-science-explained.html