The Greenland ice
cap is losing an average of 30m tonnes of ice an hour due to the climate
crisis, a study has revealed, which is 20% more than was previously thought.
Some scientists
are concerned that this additional source of freshwater pouring into the north
Atlantic might mean a collapse of the ocean currents called the Atlantic
meridional overturning circulation (Amoc) is closer to being triggered, with
severe consequences for humanity.
However, they
cannot account for the retreat of glaciers that already lie mostly below sea
level in the narrow fjords around the island. In the study, satellite photos
were analysed by scientists to determine the end position of Greenland’s many
glaciers every month from 1985 to 2022. This showed large and widespread
shortening and in total amounted to a trillion tonnes of lost ice.
“The changes around Greenland
are tremendous and they’re happening everywhere – almost every glacier has
retreated over the past few decades,” said Dr Chad Greene, at Nasa’s Jet
Propulsion Laboratory in the US, who led the research. “It makes sense that if
you dump freshwater on to the north Atlantic Ocean, then you certainly get a
weakening of the Amoc, though I don’t have an intuition for how much
weakening.”
The
Amoc was already known to be at its weakest in 1,600 years and in 2021 researchers spotted warning signs of a tipping point. A recent study suggested the collapse could happen as soon
as 2025 in the worst-case scenario. A significant part of the Greenland ice
sheet itself is also thought by scientists to be close to a tipping point of irreversible melting, with ice
equivalent to 1-2 metres of sea level rise probably already expected.
The
study, published in the journal Nature, used artificial intelligence
techniques to map more than 235,000 glacier end positions over the 38-year
period, at a resolution of 120 metres. This showed the Greenland ice sheet had
lost an area of about 5,000 sq km of ice at its margins since 1985, equivalent
to a trillion tonnes of ice.
The
most recent update from a project that collates all the other
measurements of Greenland’s ice found that 221bn tonnes of ice had been lost
every year since 2003. The new study adds another 43bn tonnes a year, making
the total loss about 30m tonnes an hour on average.
The scientists
said: “There is some concern that any small source of freshwater may serve as a
‘tipping point’ that could trigger a full-scale collapse of the Amoc,
disrupting global weather patterns, ecosystems and global food security. Yet
freshwater from the glacier retreat of Greenland is not included in
oceanographic models at present.” The influx of less dense freshwater into the
sea slows the usual process of heavier salty water sinking in the polar region
and driving the Amoc.
Prof Tim Lenton,
at the University of Exeter, UK, and not part of the study, said: “This
additional freshwater input to the north Atlantic is a concern, particularly
for the formation of deep water in the Labrador and Irminger Seas within the
subpolar gyre, as other evidence suggests these are the regions most prone to
being tipped into an ‘off’, or collapsed state.”
“That would be
like a partial Amoc collapse, but unfolding faster and having profound impacts
on the UK, western Europe, parts of North America, and the Sahel region, where
the west African monsoon could be severely disrupted,” he said. “Whether this
previously unaccounted source is enough freshwater to make a difference depends
on how close we are to that subpolar gyre tipping point. Recent models suggest
it could be close already at the present level of global warming.”
The discovery of the extra
ice loss is also important for calculating the Earth’s energy imbalance, ie how
much extra solar heat the Earth is trapping due to human-caused greenhouse gas
emissions, said Greene. “It takes a lot of energy to melt 1tn tonnes of ice. So
if we want very precise energy balanced models for the Earth, this has to be
accounted for.”
The glaciers
analysed in the study were mostly below sea level already, so the lost ice was
replaced by sea water and did not affect sea level directly. But Greene said:
“It almost certainly has an indirect effect, by allowing glaciers to speed up.
These narrow fjords are the bottleneck, so if you start carving away at the
edges of the ice, it’s like removing the plug in the drain.”
Greene
and colleagues also analysed the extent of Antarctic ice shelves over time in
a study published in 2022. It found that the total lost from the ice shelves
since 1997 was doubled to about 12tn tonnes when the shrinking areal extent of
the shelves was accounted for and added to the thinning of the shelves.
-Damian Carrington, The
Guardian
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