If you’re NOT worrying about Arctic sea ice losses you are either ignorant or insane.
Record-Thin Sea Ice Faces Big Predicted Arctic Warm-up This Week
10 May, 2017
If
you’re someone who tends to worry about Arctic sea ice losses, this
coming week’s weather forecast looks like a bit of a doozy.
And
when you consider that the sea ice is both greatly weakened and
thinned in a number of the major monitors, prospects don’t look
very good, presently, for 2017’s summer melt season as whole.
Abnormal
Warmth Over Greenland and Baffin and Hudson Bays
Over
the next 48 hours, Baffin and Hudson Bays will experience the tail
end of what an extreme warm-up that produced
exceptional May surface melt over the Greenland Ice Sheet and then
shifted westward.
Temperatures
for Hudson and Central and Southern Baffin, according to GFS model
runs, will range above freezing over this time period — hitting
as high as the low 40s (F) in Eastern sections of Hudson Bay.
Over-ocean readings (which tend to moderate, but not, apparently, in
this case) that will range from 5 to 15 degrees Celsius above
average. These rather high surface temperatures will help to kick sea
ice melt throughout these regions into higher gear.
Pacific
Side of Arctic Ocean Predicted to Heat Up
Following
the Baffin-Hudson warm-up, a large bulge of much warmer than normal
air is predicted to extend northward from a broad region extending
from Eastern Siberia through the Bering Sea and Alaska and on into
Northwestern Canada. This bulge will, according to GFS model runs, by
early next week inject periods of above freezing temperatures over a
wide region of the Arctic Ocean that includes the East
Siberian Sea,
the Chukchi
Sea and
the Beaufort
Sea.
And by this time next week, these same model runs project that 10-16
C above average temperatures will dominate a large region of the
Central Arctic — forcing above-freezing temperatures over a broad
cross-section of the North Pole zone by May 17.
(The
Arctic is expected to experience nearly 2 C above average
temperatures with some regions over the Arctic Ocean hitting 16 C [28
F] above average. These are considerable departures for May when
temperatures in the Arctic tend to moderate. So much warmth is likely
to have an impact on the already greatly thinned Arctic sea ice.
Image source: Global
and Regional Climate Anomalies.)
So
much early season warmth is likely to further impact an already
greatly weakened and thinned veil of sea ice covering the Arctic
Ocean. A cooling cap that even more conservative scientists estimate
could be completely removed during a summer as soon as the early
2030s. But in the worst case scenario, and when considering how thin
the ice is now, a nearly ice free summer could happen as soon as this
year. Few scientists really want to talk about that now — given the
likely controversy that would result. But we shouldn’t entirely
ignore that possibility for fear of backlash or criticism. Nor should
we ignore how such an event would
tend to further distort an already disrupted Northern Hemisphere
atmospheric circulation.
Indicators
Show Very Thin Ice
Over
recent weeks, sea ice area and extent measures have recovered
somewhat as temperatures over the Arctic Ocean have moderated a bit
from very warm conditions during October through March. However, a
number of indicators including
PIOMAS’s sea ice volume measure show
that despite this mild surface extent recovery, the ice is very weak
and significantly thinned.
(PIOMAS
sea ice volume measure shows a considerable record low departure
through mid April of 2017. Image source: PIOMAS.)
It’s
worth noting that a significant portion of the extent recovery over
recent weeks can be attributed to strong winds blowing ice out of the
Arctic Ocean and into the Barents
Sea as
well as out through the Fram
Strait.
Such conditions are not normally considered to be healthy ones for
ice retention through summer as ice in the Barents and Fram tends to
melt far more swiftly than ice secured in the Central Arctic. And the
Fram itself is often considered to be a graveyard for sea ice.
As
for PIOMAS,
the most recent measurement through the middle of April found that
sea ice volume had topped out at 20,600 cubic kilometers. This
measure was fully 1,800 cubic kilometers below the previous record
low set for the month. It’s a tremendous negative departure that,
if valid, shows that the state of the sea ice as of this time was
terribly unhealthy. A situation that prompted the typically
conservative Neven over
at the Arctic Ice Blog to state that it’s:
Not looking good. Not looking good at all… with a maximum that was almost 2000 km3 lower than the previous record reached in 2011, it’s obvious that anything is possible this coming melting season.
(According
to the EASE NSIDC sea ice age monitor, the multi-year sea ice is now
almost entirely removed from the Pacific side of the Arctic. Strong,
persistent winds have continued to push a good portion of the frail
remainder of this ice out toward the Fram Strait — a graveyard for
sea ice. And a big warm-up predicted for this week will begin to test
the greatly thinned ice over the Beaufort, Chukchi and East Siberian
Seas. Image source: NSIDC and The
Arctic Ice Blog.)
Moreover,
Neven last week pointed out that according a separate measure (see
image above), typically thicker multi-year ice is presently absent
from the Beaufort Sea. And, to this point, it’s worth noting that
the amazing above normal temperatures that plagued the Arctic cold
season for multiple years now have resulted in vast losses among this
most healthy subset of sea ice.
Such
considerably thinned ice presents practically no barrier to the
effects of warming. It can melt quite rapidly and it is far more
subject to the physical forces of wind and waves. With strong
southerly winds and a big warm-up now in the pipe, it appears that
this considerably thinned ice will get its first test in mid-May.
Potentially creating large sections of permanently open water very
early in the melt season and very close to the ever-more vulnerable
High Arctic.
Links:
Hat
tip to Neven and…
to
the researchers over at The
Arctic Ice Blog
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