Since the late 1970s, as global temperatures ratcheted upward, sea ice in the Arctic has been swiftly declining. But in the Antarctic sea ice continued to grow into the 2010s.

The study used data from satellites to track changes by using a brightness measurement that subtly correlates to salt content.

But because the signal is small and easily drowned out by other factors, Silvano said, it wasn’t possible to analyse them effectively until recent advances in algorithms.

When Silvano and his co-authors first noticed the rising salinity, they doubted the signal was real, suspecting an error in the satellite data. As physical measurements from ocean instruments began to confirm the trend, they realised the signal was accurate.

“Because melting ice should freshen the ocean, we thought that we should have seen freshening, right?” Silvano said.

He added that climate change is also increasing precipitation and runoff from melting glaciers in the Antarctic, which should mean more fresh water coming into the ocean’s surface.

“Instead, we saw increasing salinity.”

As the salt content increases, the density of the water changes, drawing warmer water — typically stashed deep under the surface — upward.

Hotter water causes the ice floating on it to melt and prevents it from growing back in the winter as much as it used to.

Because less sea ice means less fresh water balancing out the salinity and warmth, it’s a feedback loop that threatens greater warming, he said.

Sharon Stammerjohn, a senior research associate at the University of Colorado Boulder’s Institute of Arctic and Alpine Research, who was not involved in the research, described the paper as a sort of missing link for the potential drivers of Antarctic sea-ice changes.

“We have been struggling for about the last decade to try to figure out why Antarctic sea ice had such a rapid decline and continues to decline,” she said.

Typically, Stammerjohn said, the ocean acts as a bank of planetary heat. Because fresher water is less dense, it acts as a lid, holding back the salt and trapping heat deep below the surface.

Rising salinity means the layers of the ocean are mixing more and letting more heat escape to the surface. “Up until 2015 we kind of kept a lid on that,” she said.

Cecilia Bitz, a professor of climate science at the University of Washington, said observations of the Antarctic’s complex dynamics and vast, hard-to-access landscape remained sparse until about 10 years ago.

Then, improvements in satellite data along with a growing fleet of autonomous buoys with sensors, known as Argo floats, which provided some of the data used in Silvano’s study, began to fill in the gaps.

Recently, the United States Department of Defence announced it would be no longer be providing some of the satellite data that researchers use to monitor changes in sea ice. According to an announcement yesterday, the data will become unavailable after July 31.

“This not only affects polar researchers who rely on this for Antarctic sea ice and Arctic sea ice, but another sensor on there is key for hurricane forecasting,” Stammerjohn said.

While the details of how the scientific community might adapt when this programme is cancelled are unclear, she said, there are other satellite products, including ones maintained by the European Space Agency and the Japan Aerospace Exploration Agency, that may be able to fill the gap.

This article originally appeared in The New York Times.

Written by: Sachi Kitajima Mulkey

Photographs by: XXX

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