Ice Loss To Add 0.4C To Global Temperatures: Study

The loss of billions of tonnes of ice from Earth's frozen spaces is likely to increase global temperatures by an additional 0.4 degrees Celsius, according to research Tuesday highlighting the danger of a "vicious circle" of warming

Paris, (APP - UrduPoint / Pakistan Point News - 27th Oct, 2020 ) :The loss of billions of tonnes of ice from Earth's frozen spaces is likely to increase global temperatures by an additional 0.4 degrees Celsius, according to research Tuesday highlighting the danger of a "vicious circle" of warming.

Arctic summer sea ice levels have declined by more than 10 percent each decade since the late 1970s and mountain glaciers have shed roughly 250 billion tonnes of ice annually over the last century.

Ice loss from the West Antarctic and Greenland ice sheets is accelerating and already outstripping what scientists until recently believed to be the worst-case melt scenarios.

Decades of studies have sought to quantify how Earth's melting ice will contribute to sea level rise -- Antarctica and Greenland alone contain enough frozen water to boost oceans' height by around 60 metres.

But little research has tried to predict how ice loss will add to the already 1.0 degree C of global warming emissions from fossil fuels since the start of the Industrial Era.

Scientists at Germany's Potsdam Institute for Climate Impact Research (PIK) used a climate model that includes components on atmosphere, ocean, sea- and land-ice data to predict temperature change from ice loss under a variety of emissions scenarios.

They found that under current levels of atmospheric CO2 -- roughly 400 parts per million -- the melting of Arctic sea ice, mountain glaciers and the polar ice caps would raise temperatures by 0.4C.

That's on top of the 1.5C of warming our current emissions levels have rendered all but inevitable, and the safer cap on global warming aimed for in the Paris climate accord.

The main driver of temperature gain from ice loss would be due to a process known as albedo feedback, in which heat reflective bright ice is replaced by absorbant darker sea water and/or soil.

"If global ice masses shrink, this changes how much of the sunlight that hits the Earth's surface is reflected back into space," said lead author Nico Wunderling.