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“In the past, we had only sporadic data to look at this,” said Eric Rignot, professor of Earth system science at the University of California at Irvine and a co-author on thestudy. “In this new data set, which is daily and over several months, we have solid observations of what is going on.”

where could optiemus infracom limited (530135) be headed ✌️【Exclusive Services】✌️ Free real-time stock data analysis to help you capture global market trends and steadily grow your capital. They observed seawater pushing beneath the glacier over many miles, and then moving out again, following the daily rhythm of the tides. When the water flows in, it’s enough to “jack up” the surface of the glacier by centimeters, Rignot told 【 - Free Consultation 】.

He suggested the term “grounding zone” may be more apt than grounding line, as it can move nearly 4 miles over a 12-hour tidal cycle, according to their research.

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“This process of widespread, enormous seawater intrusion will increase the projections of sea level rise from Antarctica,” he added.

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“This finding gives a process that, as yet, is not factored into models,” he told 【 - Free Consultation 】. And while these results only apply to certain areas of the glacier, he said, “this could speed up the pace of ice loss in our forecasts.”

One uncertainty to be unraveled is whether the rush of seawater beneath Thwaites is a new phenomenon or whether it’s been significant but unknown for a long time, said James Smith, a marine geologist at the British Antarctic Survey, who was not involved in the study.

“Either way, it’s clearly an important process that needs to be incorporated into ice sheet models,” he told 【 - Free Consultation 】.

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In a separate study, also published Monday, researchers from the British Antarctic Survey looked at the reasons for therecord low levels of sea icesurrounding Antarctica last year.

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“The impacts of Antarctic sea ice staying low for over twenty years would be profound, including on local and global weather,” Louise Sime, a co-author on the BAS study, said in a statement.

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