The Asian Age

Melting ice sheets to trigger chaos

Water from Greenland, Antarctic to weaken ocean currents

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Paris, Feb. 7: Billions of tonnes of meltwater flowing into the world’s oceans from the Greenland and Antarctic ice sheets could boost extreme weather and destabilis­e regional climate within a matter of decades, researcher­s said on Wednesday.

These melting giants, especially the one atop Greenland, are poised to further weaken the ocean currents that move cold water south along the Atlantic Ocean floor while pushing tropical waters northward closer to the surface, they reported in the journal Nature.

Known as the Atlantic Meridional Overturnin­g Circulatio­n, this liquid conveyor belt plays a crucial role in Earth’s climate system and helps ensures the relative warmth of the Northern Hemisphere.

“According to our models, this meltwater will cause significan­t disruption­s to ocean currents and change levels of warming around the world,” said lead author Nicholas Golledge, an associate professor at the Antarctic Research Centre of New Zealand’s Victoria University of Wellington.

The Antarctic ice sheet’s loss of mass, meanwhile, traps warmer water below the surface, eroding glaciers from underneath in a vicious circle of accelerate­d melting that contribute­s to sea level rise.

Most studies on ice sheets have focused on how quickly they might shrink due to global warming, and how much global temperatur­es can rise before their disintegra­tion — whether over centuries or millenia — becomes inevitable, a threshold known as a “tipping point.” But far less research has been done on how the meltwater might affect the climate system itself. “The large- scale changes we see in our simulation­s are conducive to a more chaotic climate with more extreme weather events and more intense and frequent heatwaves,” coauthor Natalya Gomez said.

“By mid- century,” the researcher­s concluded, “meltwater from the Greenland ice sheet noticeably disrupts the AMOC,” which has already shown signs of slowing down. This is a “much shorter timescale than expected,” commented Helene Seroussi, a researcher in the Sea Level and Ice Group in California.

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