Underwater
glacial melting up to 100 times faster than thought, study finds
Existing
models are ‘wildly inaccurate’ and significantly underestimated
extent of melting, scientists say
25
July, 2019
Underwater
glacial melting is happening up to 100 times faster than previously
thought, a major study has found.
For
the first time, researchers directly measured the melting of
tidewater glaciers below the waterline.
They
found existing models were “wildly inaccurate”.
Study
co-author Rebecca Jackson, of Rutgers University-New Brunswick in the
US, said: “We found that melt rates are significantly higher than
expected across the whole underwater face of the glacier – in some
places 100 times higher than theory would predict.”
Until
now, scientists did not know how fast these glaciers – which are
found in Greenland, Alaska and Antarctica – were melting under the
surface.
Researchers
previously used water and air temperature, as well as ocean currents,
to measure the melt speed.
But
the latest study, published in the journal Science,
found that ocean salinity and the shape of the glacier was also
important.
“We
have opened the door to correcting these models and allowing other
researchers to use our method to explore other tidewater glaciers
around the world," lead researcher Dr David Sutherland told The
Independent.
LeConte Glacier,
which flows into LeConte Bay (NOAA)
The
oceanographer, from the University of Oregon, added that his
team's data “provides a new constraint for improving
those models and points to the ocean as an important trigger for ice
loss”.
Scientists
studied the underwater melting of LeConte Glacier, which flows into
LeConte Bay in south Juneau in Alaska between 2016 and 2018.
They
used sonar to scan and profile the underwater face of the glacier.
They also measured the speed of currents, temperature and salinity of
the meltwater flow.
Iceberg
calving was detected using time-lapse photography, and weather
station data measured surface melt. The team believe
their approach could be used to study melting rates at other types of
glaciers.
This
latest study adds to research that suggests assumptions about
underwater melting at glaciers need to be revisited – because of
the alarming effects of the phenomenon on rising sea levels.
Dr
Sutherland added: “Future sea-level rise is primarily determined by
how much ice is stored in these ice sheets. We are focusing on the
ocean-ice interfaces because that’s where the extra melt and ice is
coming from that controls how fast ice is lost.
“To
improve the modelling, we have to know more about where melting
occurs and the feedbacks involved.”
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