Drastic Antarctic sea ice loss could fuel extreme weather in years ahead

Drastic Antarctic sea ice loss could fuel extreme weather in years ahead

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Heat loss from the Southern Ocean to the environment as an outcome of sea ice loss might add to stormier weather condition and modifications in ocean flow.
(Image credit: Sergio Pitamitz/VW Pics/Universal Images Group through Getty Images)

Disappearing Antarctic sea ice might result in more storms in the Southern Ocean, brand-new research study programs.

Researchers discovered that decreased Antarctic sea ice protection in 2023 triggered the ocean to lose additional heat to the environment. That heat loss might interrupt ocean flow currents and trigger more regular storms in locations where sea ice protection has actually decreased.

In 2015, ice protection come by almost half compared to the average in between 1990 and 2015 in 4 locations: the Bellingshausen Sea and the external Weddell and Ross seas, where sea ice reduced by approximately 80 %, and Enderby Land, which saw a drop of as much as 50 %. The complete dataset from 2024 isn’t offered yet, however continued low protection recommends a continuous pattern.

“It is too early to state whether 2023 and its record-breaking sea-ice decline marks the onset of a fundamental shift in the amount of Antarctic sea ice,” research study co-author Simon Joseyan oceanographer at the National Oceanography Centre in the U.K., stated in a declaration “However, our study does reveal the extreme conditions to be expected in future years of low ice regrowth, with 2024 looking like it is continuing the sharp change seen in 2023.”

Related: ‘We remained in shock ‘: Antarctica is acting in such a way we’ve never ever seen before. Can it recuperate?

To comprehend the effect of this extreme sea ice loss, scientists evaluated heat flux in between the air and sea, in addition to modifications in ice protection from Antarctica in 2023. In the research study, released Dec. 18 in the journal Naturethe scientists discovered that the recently exposed ocean surface area lost heat almost one and a half times quicker than it had in previous years.

This boost in heat loss might have significant effects. Heat loss cools water near the ocean surface area, triggering it to end up being denser than in previous years. As this thick surface area water sinks, it might interfere with much deeper ocean currents and flow in the Southern Ocean.

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“This cooling and subsequent sinking of waters previously covered by sea ice has the potential to release deeper warm waters that would normally be kept away from ice by an insulating surface layer. In turn, this has the potential for increasing sea ice melt in future years,” research study co-author Andrew Meijersan oceanographer with the British Antarctic Survey, stated in the declaration.

Modifications in heat flux in between the ocean and the environment might likewise add to more regular storms over Antarctica as the environment uses up more heat. By thinking about the variety of days with high winds as a proxy for storm frequency, the scientists discovered approximately 11.6 rainy days in June and July 2023 over a couple of various areas of ice loss, up from approximately 9.1 rainy days in between 1990 and 2015. Some locations, like the northern Weddell Sea, saw as much as 7 extra rainy days monthly.

Previous research study recommends that Antarctic sea ice melting might likewise impact temperature levels around the remainder of the world. “Our research highlights the need to keep studying the link between Antarctic sea ice loss, ocean heat loss, and changing weather patterns,” Josey stated in the declaration. “These changes could affect weather and climate far beyond Antarctica.”

Skyler Ware is a freelance science reporter covering chemistry, biology, paleontology and Earth science. She was a 2023 AAAS Mass Media Science and Engineering Fellow at Science News. Her work has actually likewise appeared in Science News Explores, ZME Science and Chembites, to name a few. Skyler has a Ph.D. in chemistry from Caltech.

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