What the breakaway Spalte glacier tells us about climate change
Scientists warn that calving of largest remaining Arctic ice shelf could be ‘major centre of action for the deglaciation of Greenland’
A segment of the largest ice shelf in the Artic has broken off and shattered into small pieces, with scientists claiming the incident is further evidence of climate change’s effect on the region.
This week, the 42 square mile Spalte Glacier in northern Greenland separated from the Nioghalvfjerdsfjorden ice shelf in a dramatic calving event, with satellite images revealing that the glacier has since become a “flotilla of icebergs”, BBC News reports.
Researchers believe the loss of the ice chunk is a direct result of rapid climate change taking place in the Arctic around Greenland.
Speaking to the BBC, Dr Jenny Turton said: “The atmosphere in this region has warmed by about 3C since 1980... And in 2019 and 2020, it saw record summer temperatures.”
So what has happened in Greenland and what does it say about climate change?
What is the Nioghalvfjerdsfjorden ice shelf?
Also known as 79N, the Nioghalvfjerdsfjorden ice shelf is one of the largest in the world at around 80km long by 20km wide and plays an important role in regulating the Arctic climate around Greenland.
According to a 2018 paper published in the journal Nature, the shelf - together with its neighbours Zachariæ Isstrom and Storstrommen - is one of the major outlets of the North East Greenland Ice Stream (NEGIS), a 600-km-long ice stream that drains around 15% of the interior Greenland ice sheet into the ocean.
However, while the ice shelf was thought to be relatively stable, “increased thinning rates” seen on the shelf since 2006 are “likely related to increased air temperatures leading to higher melt rates and a reduction in summer sea ice concentration”, which “facilitates higher calving and retreat rates”.
What happened this week?
The BBC reports that at its leading edge, the 79N ice shelf split in two, with a “minor offshoot turning directly north” known as the Spalte Glacier.
After enduring high summer temperatures last year and fracturing heavily as a result, it fully broke off from the remainder of the ice shelf this week, fragmenting into thousands of small icebergs.
What does this say about climate change?
“Look closely at the satellite pictures and the higher air temperatures recorded in the region are obvious from the large number of melt ponds that sit on top of the shelf ice,” the BBC reports, adding that the presence of such pools of water is often problematic for ice platforms as they push down through the ice and weaken it structurally.
The broadcaster adds that oceanographers believe the ice sheet is “being attacked from above and below” after also documenting warmer sea temperatures, meaning the shelf ice is almost certainly being melted from beneath.
The paper published in Nature says the ice shelves that make up the NEGIS region, if lost, have the potential to see global sea levels rise by 1.1m.
And this week’s event is far from the only damning piece of evidence that climate change is adversely affecting Greenland.
In a 2015 study, scientists from the Danish Meteorological Institute analysed data from 11 stations around Greenland and found that all stations showed a positive correlation between warmer summers and an increased rate of ice sheet loss.
“79N became ‘the largest remaining Arctic ice shelf’ only fairly recently, after the Petermann Glacier in northwest Greenland lost a lot of area in 2010 and 2012,” Professor Jason Box of the Geological Survey of Denmark and Greenland (GEUS) told the BBC this week.
“What makes 79N so important is the way it’s attached to the interior ice sheet, and that means that one day - if the climate warms as we expect - this region will probably become one of the major centres of action for the deglaciation of Greenland.”