Immersible uncovered secret structures. Then she disappeared under Antarctic waters.

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  • In 2022, an international team of scientists sent an autonomous underwater vehicle with a length of 20 feet (AUV), called “RAN” to move to the endless region under Dotson’s ice shelf in Western Antarctica.

  • The resulting study revealed the complex dynamics that leads to faster melting speeds between the western and eastern parts of the ice shelf.

  • After returning to the area in 2024 in the catalog of changes in the ice shelf, Ran was lost under the icy waves, a dumb failure to explore this critically important, climate-stressed area.


When you come up with a solution, it helps to approach a problem from every possible angle. The same can be said of an ice melt caused by the climate in Antarctica, which is why the international cooperation of the Thwaites (ITGC) Glacier programming an automated underwater vehicle (AUV)-an Antimen “RAN”-to immerse the Ice Cavity.

For 27 days, the submarine has traveled more than 600 miles-10 miles directly into the cavity itself-to understand the mechanics about how glaciers melt faster near strong underwater currents and to watch the topography of this most important ice shelf. What the experts behind this submersible have found that the attributes on the western part of the Ice Shelf differ significantly with the eastern part, which is larger and therefore melts more slowly.

Visualization of tear -shaped areas under Dotson’s ice shelf. Philip Sted/University in Gotheburg

RAN AUV also produces high resolution cards on the underside of Dotson Ice Shelf, which reveal strange characteristics of tears, ice plateau and detailed erosion patterns. The study results were published last week in the magazine Science is progressingS



“We have used satellite data and ice cores earlier to observe how glaciers change over time,” Anna Welin, a lead author of the study, said in a press statementS “As we navigate the submersible in the cavity, we were able to get high -resolution cards on the icy lower side. This is a bit like seeing the back of the moon.”

Unlike the glaciers that rest on the land, the ice shelves are actually part of the ocean. They somehow act as a fortress, which protects the ice on the land from flowing into the ocean and raising sea level and are vital to these polar ecosystems as a result. And since these shelves are resting on the ocean, you may fall under them.

But being possible does not mean it’s easy.

diagram

Review of the RAN AUV mission. Anna Wåhlin/Science Advances

The 20-foot RAN submersible in the ice waves (Advanced Multiveam Sonar) on the ice to map its characteristics, but due to their sub-subcontarct location, Wåhlin and its team could not communicate with AUV or track their movements with GPS. After 14 missions – some for several hours, while others extended longer than one day – about 50 square meters of ice were mapped, and the depicted structures were more complicated than someone imagined.

“Mapping gave us a lot of new data that we need to look at more closely,” Velin said in a press statement. “It is clear that many previous assumptions about the melting of the glacial lower sides fall out. Current models cannot explain the complex models we see. But with this method we have a greater chance of finding the answers.”



One of the findings of the team is that the different degrees of the melt between the east and the western part of the Ice Shelf of Dotson can be explained by a phenomenon known as a modified circuits of deep water (MCDW), which is when the Pacific and Indian Ocean is mixed with other local water tables. These data were supplemented by the RAN measurements of these underwater currents, as well as the high speeds of melting fractures that pass through the glacier.

Although the team’s initial mission was to study the nearby Thwaites glacier, the environment turned out to be too difficult to access. However, Dotson’s Ice Shelf serves as a perfect candidate for equipment and method testing as per The New York TimesS These studies were conducted in 2022, and the team returned earlier this year to see what changes in the ice shelf have occurred. The worst fears of Wåhlin and her team were realized then no come up at the pre -planned meeting pointS The team suspects that AUV was either moving or the target of some curious seals.

“Although we received valuable data, we did not receive everything we had hoped. These scientific achievements became possible thanks to the unique submersible, which was it,” Verlin says in a statement from the press. “This study is necessary to understand the future of Antarctica’s ice sheet and we hope to be able to replace RAN and continue this important work.”

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