Nathaniel B. Palmer, a glacier, mapped more than 2,000 square kilometers of sea floor in front of the glacier.

This Antarctic colossus is melting at a rapid rate, dumping billions of tons of ice into the oceans each year, raising global sea levels.

Now, the UK-US team has surveyed the deep sea lanes in front of the glaciers that provide access to almost certainly warm water to infiltrate and attack the area below the Thwaites.

Dr. Kelly said: “The details of these channels have never been mapped before, and what we’ve found is that they’re actually bigger than anyone – deep00m. Deep up Think back to six footballs, ”said Dr. Kelly. Hogan from the British Antarctic Survey (BAS)

“And because it’s so deep and wide – it can get a lot of water and melt because of the floating front of the Thwaites as well as the ice on the beach,” she told BBC News.

It’s a gorgeous view, with its vibrant front, or “ice shelf”, pushing away to the sea and pulling out huge icebergs. But satellite surveillance shows that this glacier is melting at a rapid rate.

In the 1990s and 1990s, it was losing only 10 billion tons of ice a year. Today it is more than 1 trillion tons. The reason behind the melting is the relatively warm bottom water flow drawn from the wide ocean.

Currently, the loss of ice in Thwaites contributes about 4% to the annual increase in global sea level, with a total increase of 65 cm expected if the entire glacier collapses.

No one thinks this will happen in the short-to-medium term, but Thawites are considered particularly vulnerable in the warming world, and scientists know how fast any changes can happen.

His scientists took the ship, equipped with echo-sounders, to the icebergs of the glacier to explore the shape of the ocean below.

The plane also went beyond the cupboard to measure small changes in gravitational pull. These deviations reflected the ondules of the seafloor beneath the shelf.

The two combined datasets now provide the best view of the basic migration of thwites. They find their way into the deep channel mesh that forms a rigid piece before joining the main cavity under the ice cap.

“The connected channels we mapped in detail for the first time are potential ways to get into the warm waters of the deep ocean and cause damage where glaciers are still starting to rise where the seashore is. And “Float,” BAS colleagues said. Tom Jordan explained, “But to melt the base of the ice shelf, if you weaken, the ice in the glacier flow will go even higher.”

Scientists need real-world data to learn about their models so that they can get realistic conclusions when they simulate possible future behavior.

The new information refines the volumes to be mixed in warm water which may be considered possible under different conditions.

While surveying them, scientists also now have a better idea of ​​the general roughness of the ocean floor.

This tells them about the further rapid motion of ice in a glacier that causes it to slide across rocks and mud. What the researchers have created, if you like, is a kind of “stickiness index” to keep computer models extra limited.

At the moment, the east side of the ice shelf is stuck on a large ridge, which gives it stability. But the current melting trend suggests that the situation will not last long, says Dr. Robert Larter of BAS.

“When the former ice shelf is unpinned, the ice will spread and thin and eventually break, because we see this happening right now on the tongue of the glacier in the middle. “Before the ice shelf break-up, unpinning and thinning will reduce the butterfly effect of the shelf at the top of the glacier, resulting in increased ice flow. This will cause the glacier to shrink and the grounding line to retreat even faster.”

This Australian summer was due to the team going to the glacier, but the remoteness of that location means that the risks are very high if someone falls ill. Once the coronavirus has been properly treated, scientists will return.

Dr. Hogan said: “It’s amazing to see the change happening in places like Thawites. “When we were in 201, we were able to reach the ice cap and we were able to do that, and the reason for our observations is that the historically ever-present glaciers and sea-ice are starting to disappear.”

New documents in The Cryosphere have been published in two papers and are accessible Here And Here.

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Glacier, Thwaites Glacier, Antarctica, Nathaniel B. Palmer

World news – GB – Thwits: ‘Doomsday Glacier’ weakness is seen in new maps

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