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The world's largest ice shelf melts 10 times faster than expected, while the ocean absorbs the heat of the sun
- The Ross ice floe is a floating ice sheet that is advancing in the Antarctic Ocean
- The loss of ice patches causes the acceleration of glaciers as it removes a barrier
- In 4 years, researchers measured temperature, salinity, melting rate and currents
- The instruments showed that the surface water heated by the sun flowed into the cavity under the pack ice, which almost tripled the melting rates in summer.
A study shows that some of the world's largest pack ice melts 10 times faster than expected due to the warming of the sea that surrounds it.
The Ross ice floe, a floating Antarctic ice sheet the size of France moving forward in the ocean, is more vulnerable to global warming than previously thought.
The results suggest that surface water heated by the sun also plays a crucial role in ice melting, as well as in their exposure to the warm waters of deep oceans, as is often thought.
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A study shows that some of the world's largest pack ice melts 10 times faster than expected due to the warming of the sea that surrounds it. The discovery suggests that Ross ice floes are more vulnerable to global warming than previously thought.
After reviewing the data collected over the last four years, the researchers found that the water was flowing under the pack ice, which almost tripled summer melting rates.
Loss of pack ice removes barriers to glaciers that carry water to the ocean, allowing sea level rise.
The team from Cambridge University spent several years studying the interactions between the northwestern Ross Sea ice and the ocean below.
Dr. Craig Stewart, a former Cambridge scientist, currently at the National Institute of Water and Atmospheric Research (NIWA), said: "It is generally thought that the stability of ice platforms is related to their exposure to the deep warm waters of the ocean.
However, he and his team have found that surface water heated by the sun also plays a "crucial role" in melting ice.
The team measured temperature, salinity, melting rate and ocean currents using instruments drilled through a 260-meter borehole.
Four years of data were also collected in an oceanographic mooring under the pack ice.
In addition, a custom radar system was used to monitor changes in ice thickness.
The instruments showed that the surface water heated by the sun flowed into the cavity under the pack ice, which almost tripled the melting rates in summer.
The results suggest that surface water heated by the sun also plays a crucial role in ice melting, as well as in their exposure to the warm waters of deep oceans, as is often thought. By looking at the four-year data, the researchers found that this water was flowing under the ice.
Dr. Stewart added, "Climate change is likely to result in a decrease in sea ice and an increase in sea surface temperature in the Ross Sea, suggesting that melting rates in this region will increase at sea level. # 39; future. "
Dr. Poul Christoffersen, of Cambridge University, pointed out that the collapse of ice platforms can double or triple the rate at which glaciers flow into the ocean.
"The difference here is the sheer size of Ross's pack ice, which is more than 100 times larger than the pack ice that we've already seen disappear," he said.
"The observations we made at the front of the ice floe have direct consequences for many large glaciers flowing into the pack ice, some up to 900 km."
The results are published in the latest issue of Nature Geoscience.
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