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What is underneath the Antarctic ice sheet?

What is underneath the Antarctic ice sheet?

The lakes grow and shrink beneath the ice. Scientists have discovered two new lakes buried deep beneath the Antarctic Ice Sheet. These hidden gems of frigid water are part of a vast network of ever-changing lakes hidden beneath 1.2 to 2.5 miles (2 to 4 kilometers) of ice on the southernmost continent.

What is trapped in the layers of snow packed in ice sheets?

Ice sheets are made up of layers of snow and ice that collected over millions of years. Those layers contain trapped gases, dust, and water molecules that scientists can use to study past climates.

What is the difference between an ice shelf and an ice sheet?

Ice sheets are large (over 50,000 square kilometers) masses of ice that cover land and feed into ice shelves via glaciers. Ice shelves are extensions of ice sheets: the part of the ice sheet that floats on the water. Basically, ice sheets flow off land onto the ocean; the floating parts are ice shelves.

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How old is the oldest ice ever cored?

2.7-million-year-old
Clues to ancient atmosphere found in bubbles trapped in Antarctic samples. Scientists announced today that a core drilled in Antarctica has yielded 2.7-million-year-old ice, an astonishing find 1.7 million years older than the previous record-holder.

When was the last time Antarctica was ice free?

about 34 million years ago
It was ice-free until about 34 million years ago, when it became covered with ice. The lowest natural air temperature ever recorded on Earth was −89.2 °C (−128.6 °F) at the Russian Vostok Station in Antarctica on 21 July 1983.

Has Antarctica always been frozen?

Antarctica hasn’t always been covered with ice – the continent lay over the south pole without freezing over for almost 100 million years. The warm greenhouse climate, stable since the extinction of the dinosaurs, became dramatically colder, creating an “ice-house” at the poles that has continued to the present day.

How much of the Greenland ice sheet has melted?

From September 1968 to August 2021, the Greenland ice sheet has lost around 5,500 gigatons of ice — equivalent to 1.5 centimeters of global average sea level rise.

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What is the difference between ice sheet and glacier?

Basically, glaciers originate on land, and ice floes form in open water and are a form of sea ice. Glaciers that extend in continuous sheets and cover a large landmass, such as Antarctica or Greenland, are called ice sheets.

Why are ice shelves collapsing?

Scientists attributed rapid ice shelf collapse to warmer air and water temperatures, as well as increased melt on the ice shelf surface. Retreating sea ice may also play a role.

Why is the ice in Antarctica blue?

A fallen meteorite in Antarctica is quickly covered by snow and buried in one of the great Antarctic glaciers. The glaciers slowly move toward the ocean, and their ice turns blue because all its air bubbles are squeezed out.

How old was the bottom of the ice core she was talking about?

It was expected that the lower temporal resolution records would extend beyond ~100,000 years before present, but it was a big surprise to many that the oldest ice at the bottom of this core was less than 70,000 years old.

What was Antarctica like before it froze?

A new paper reveals that the frozen continent of Antarctica was once a temperate rainforest. This dramatic difference in climate was due to high levels of CO2 that managed to maintain mild weather even through months when the sun didn’t shine on this part of the world.

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What are ice sheets and why are they important?

Ice sheets contain a record of hundreds of thousands of years of past climate, trapped in the ancient snow. Scientists recover this climate history by drilling cores in the ice, some of them over 3,500 meters (11,000 feet) deep.

Why do scientists study the layers of the snow cycle?

The season turns cold and dark again, and more snow falls, forming the next layers of snow. Each layer gives scientists a treasure trove of information about the climate each year. Like marine sediment cores, an ice core provides a vertical timeline of past climates stored in ice sheets and mountain glaciers.

How do scientists measure the temperature of ice sheets?

Scientists can confirm these chemistry-based temperature measurements by observing the temperature of the ice sheet directly. The ice sheet’s thickness makes its temperature much more resistant to change than the six inches of snow that might fall on your driveway during a winter snowstorm.

How does snow affect the Earth’s climate?

Because of their light color, snow and ice also reflect more sunlight than open water or bare ground, so a reduction in snow cover and ice causes the Earth’s surface to absorb more energy from the sun and become warmer.