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Why Antarctica and the Arctic are polar opposites

Author: Douglas Fox / Source: Science News for Students

an aerial photo showing melt ponds on Arctic sea ice, there are two researchers in the middle of the image
Melt ponds form on Arctic sea ice during the summer. Their being dark increases how much of the sun’s heat they will absorb (not reflect), speeding the rate at which they melt.

The Arctic and Antarctic are the two coldest regions on Earth. Sitting at opposite poles, they might seem like mirror images of each other.

But their environments are shaped by very different forces. And that’s why global warming is affecting them in very different ways.

These differences also help explain their effects on the rest of the planet.

an animated gif showing the changes in ice and sea ice during part of 2014 in the Arctic and Antarctic
These side-by-side maps show changes in ice and sea ice in the Antarctic and the Arctic in 2014. Differing geography is one reason these two regions respond somewhat differently to Earth’s global warming.

At the north end of the world, the Arctic consists of an ocean enclosed by several large blocks of land: North America, Greenland, Europe and Asia.

Much of the Arctic Ocean is covered by a thin crust of sea ice, most of it 1 to 4 meters (3 to 13 feet) thick. It forms as the surface of the ocean freezes during winter. Some of this ice melts during the warm months. Arctic sea ice reaches its smallest area at the end of summer, in September, before it starts growing again.

Arctic sea ice has shrunken dramatically in recent years. The area of ice left at the end of summer is now about 40 percent less than it was in the early 1980s. Each year, on average, it decreases by another 82,000 square kilometers (32,000 square miles) — an area about the size of the state of Maine. The pace of sea-ice loss has “surprised a lot of people,” says Julienne Stroeve.

She’s a polar scientist at the University of Manitoba in Canada. And she predicts that by 2040 the Arctic Ocean could be mostly ice free during summer.

The situation in Antarctica, at the south end of the world, is quite different. The sea ice here actually has increased a bit since 1980. This often confuses people. And climate skeptics sometimes take advantage of this confusion to mislead people. Those skeptics argue that the world is not actually getting warmer. They cite expanding Antarctic sea ice as evidence of this. But if you understand how the Arctic and Antarctic are different, then what’s happening down south makes sense.

Opposite personality

Antarctica is in some ways the opposite of the Arctic. Rather than water surrounded by land, it is land surrounded by water. And that difference has shaped the climate of Antarctica in major ways.

The Southern Ocean, which surrounds Antarctica, is the only place where a ring of ocean, unbroken by land, circles the planet. If you’ve ever crossed the Southern Ocean by ship, you will know it is some of the roughest water on Earth. The wind constantly whips the water into waves that can tower 10 to 12 meters (33 to 39 feet) — as tall as a three-story building. That wind always pushes the water eastward. It creates an ocean current that circles Antarctica. Such a current is known as circumpolar.

The Antarctic Circumpolar Current is the most powerful ocean current on the planet. It, and the winds that drive it, isolate Antarctica from the rest of the world. They keep Antarctica far colder than the Arctic.

The Arctic and parts of Antarctica are among the fastest-warming places on Earth. They are warming up to five times as quickly as the rest of the planet….

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