'Attacked
from two sides': Antarctic sea ice hits another record low
Blue iceberg floating in the sea near Cierva Cove on the Antarctic Peninsula.
SMH,
27
September, 2017
Sea
ice around Antarctica has shrunk about 2 million square kilometres in
just three years, swinging from a record large maximum area covered
to a record low, in a shift that could have implications for the
global climate.
While
a late burst in ice cover this spring cannot be ruled out, it appears
the sea ice around Antarctica has peaked for the sea at about 18.013
million square kilometres, the smallest maximum extent in the 30-plus
years of satellite readings, Jan Lieser, from the Antarctic Climate
and Ecosystems CRC, said.
Trillion-tonne
iceberg breaks off Antarctica
As
big as Bali, the loss of the Larsen C ice shelf will require maps to
be redrawn and could ultimately cause sea levels to rise.
"It
looks like we have passed the peak," Dr Lieser told Fairfax
Media, adding the sea ice "is being attacked from two sides",
from above and below.
For
Antarctica, the lowest maximum extent, recorded on September 12,
follows a record low minimum sea ice coverage recorded on March 1
after the summer thaw, he said.
As
with the Arctic, the warming oceans are undercutting sea ice from
below, while the warming atmosphere is melting ice from above.
Global Sea Ice barrel August 2017 #GlobalWarming #ClimateChange
Antarctica's
variability, though, makes it a more complex problem to understand
than its polar opposite.
For
instance, the freshwater from melting land-based glaciers more
readily freezes than salty sea water, increasing sea ice in some
regions of the continent.
Altered
precipitation patterns can also lead to extra snow, adding depth to
both land and sea ice.
Zack
Labe, an ice researcher at the University of California, Irvine,
cautioned against a definitive call that maximum sea ice coverage had
been reached this year.
Melting
is going on at both ends of the planet, with Antarctic and Arctic sea
ice extents reaching record lows in the past year. Photo: Richard
Harker\
He
noted the first week of October in 2015 had a large net increase of
sea ice after an extended retreat. (See chart below from the US
National Snow and Ice Data Center.)
"Antarctic
sea ice extent is particularly variable day-to-day, given weather
conditions, and it's worth waiting another week," Mr Labe said.
Those
conditions include wind and wave action that can bunch sea ice or
spread it out.
John
Turner, a research scientist with the British Antarctic Survey, said
the September 12 maximum reading - which he put at 18.023 million
square kilometres - looks to have been the peaked. That would place
it at slightly less than the previous smallest maximum of 18.027
million square kilometres in 1986.
"This
year's maximum is a far cry from the 20.201 million square kilometres
record maximum we had in 2014 and shows the highly variable nature of
sea ice around the Antarctic continent," Dr Turner said.
"[On
25 September], the ice extent had fallen to 17.689 million square
kilometres so it's highly unlikely that the extent will increase by
much over the next few weeks and we can assume that we've seen this
year's maximum."
Climate
signals
Even
if the record low maximum wavers slightly, the Antarctic sea coverage
is well shy of the average of about 19 million square kilometres over
the past three decades or so, Dr Lieser said.
(See
the latest NASA satellite image of Antarctica below.)
While
the climate change signal is much clearer in the northern latitudes -
where longer-term records show a relatively steady retreat of Arctic
sea ice - evidence of global warming's impact around Antarctica is
also showing up in the observations.
"We
see an increase in the storminess of the Antarctic, and that's
obviously redistributing the sea ice around" the continent
differently, Dr Lieser said.
"Maximum
sea ice extent is attributed to that change in wind patterns."
The
storms can also have an impact "far and wide", including on
Australia's weather, he said.
Scientists
are less sure of the trends in sea ice volume in the southern
hemisphere than in the north, given the difficultly satellites have
in distinguishing sea ice from the snow that has accumulated on it,
for instance.
'Conveyor
belts'
Understanding
such processes, though, is "critically important to
understanding the climate of the earth" because of the way sea
ice formation works as the initial driver of the global ocean
"conveyor belts", Dr Lieser said.
When
sea ice forms, brine from salty sea water is expelled. As it sinks by
gravity, it draws in surface water, helping to disseminate warm
tropical heat towards the poles.
There
is no sign yet of a slowing in the major over-turning circulation
belts, such as the Gulf Stream that transports warmth from the Gulf
of Mexico to northern Scandinavia, keeping that region much more
habitable.
Still,
climate models suggest the belts could weaken or change course in the
future, Dr Lieser said.
Disturbing
one variable in such complex systems can have "major
implications" on the global climate, he said.
(See
US National Oceanic and Atmospheric Administration chart below of
percentage changes of sea ice concentration in September, compared
with previous years in the satellite era.)
Dr
Lieser is one of more than 60 representatives from 12 countries
gathered this week in Hobart to discuss sea ice, including how it is
beginning to affect ship traffic
"We
have seen a number of private and commercial ships becoming stuck in
the Antarctic sea ice in recent years, which have led to costly
rescue operations that can delay scientific work," he said.
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