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Don't Look Now, but Arctic Sea Ice Mass has
Grown almost 40% since 2012
Sunday, October 01, 2017 by: Tracey Watson📉
One of the most popular pieces of "evidence" that climate
alarmists just love to bring up to prove the global warming narrative
is the "all the ice is melting in the Arctic and the polar bears are
dying" line. We've all seen the documentaries where a polar bear
is desperately clinging to a tiny piece of ice and you just know
he's going to die soon. But is any of it really true? What does the
latest science really say about the ice in the Arctic circle?
Earlier this month, Climate Depot reported that the latest
figures from the National Snow and Ice Data Center, located at the
University of Colorado, show that sea ice extent has increased by 40
percent since 2012. The Danish Polar Portal, which
monitors ice and climate in the Arctic, reported on the 12th of
September this year:
There has been quite some discussion about Greenland in the
climate blogosphere this year. Heavy snow and rain in winter with a
relatively short and intermittent summer melt season have left the
Greenland ice sheet with more ice than has been usual over the last
twenty years - in fact we have to go back to the 1980s and 90s to
see a year similar to this one in terms of snow fall and ice melt,
though perhaps not for iceberg calving. Š
This has been the pattern in the Arctic over the last few years.
Back in 2015, BBC News
reported that Arctic ice had grown by a staggering 30 percent after
what they called an "unusually cool summer" - 'unusual' indeed,
if the global warming narrative is to be believed. That trajectory
continued into 2014, and the increases in ice for those two years
exceeded all recorded losses in the preceding three years. That 30
percent constituted a massive amount of physical land area -
the Daily Mail reported at the
time that a cooler Arctic summer had left over 530,000 additional
square miles of ice than the previous year.
Astoundingly, the mainstream media, in spite of having this
information at their fingertips, continues to spout the same old
global warming story. In the very same BBC article cited earlier, for example,
the writer immediately insisted that "2013 was a one-off" and went
on to stress that the Arctic region had warmed more than most other
places on Earth over the past three decades.
(CLIP.....)
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BBC: Arctic Ice 'Grew by a Third' after Cool
Summer in 2013
By Matt McGrath
Environment correspondent, BBC News
(Ecxerpt) This polar monitoring
spacecraft has a sophisticated radar system that allows scientists to
accurately estimate the volume. The researchers used 88 million
measurements of sea ice thickness from Cryosat and found that between
2010 and 2012, the volume of sea ice went down by 14%. They
published their initial findings at the end of 2013 - but have now
refined and updated them to include data from 2014 as well.
Relative to the average of the period between 2010 and 2012,
the scientists found that there was a 33% increase in sea ice volume
in 2013, while in 2014 there was still a quarter more sea ice than
there was between 2010 and 2012.
"We looked at various climate forcing factors, we looked at
the snow loading, we looked at wind convergence and the melt season
length of the previous summer," lead author Rachel Tilling, from
University College London, told BBC News.
"We found that the the highest correlation by far was with the
melt season length - and over the summer of 2013, it was the coolest
of the five years we have seen, and we believe that's why there was
more multi-year ice left at the end of
summer."
(CLIP....)
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End of the SMB Season Summary
2017
12 Sept 2017
As the Surface Mass Budget (SMB) year ends, it's time for our
now traditional look-back at the season since the 1st September
2016. There has been quite some discussion about Greenland in the
climate blogosphere this year. Heavy snow and rain in winter with a
relatively short and intermittent summer melt season have left the
Greenland ice sheet with more ice than has been usual over the last
twenty years - in fact we have to go back to the 1980s and 90s to
see a year similar to this one in terms of snow fall and ice melt,
though perhaps not for iceberg calving.
At the end of the SMB year that started on the 1st September
2016 and went through to the 31st August 2017, and not including
the loss of icebergs, about 544 Gt more snow fell on the surface of
the ice sheet than melted and ran into the ocean, compared to an
average for 1981 to 2010 of about 368 Gt at the same point in the
year. Note that this figure and the surface mass budget in
general do not account for calving losses and the submarine melt of
glaciers. Together calving and submarine melt have averaged around 500
Gt of ice loss per year over the last two decades. The end of year
surface mass budget is therefore rather high for the 2000s and the
1990s, though it's not the highest in the record and 2016-2017
has therefore not been a record year for Greenland ice sheet mass
balance. If we rank the annual surface mass balance since 1981 from
low to high, the lowest on record was 2011-2012 (38 Gt) and this year
is the 5th highest out of the 37 year record. The highest on
record 1995-1996 had an end of year SMB of 619 Gt in our
records.
So what has contributed to this high SMB this year? As we
have written previously, Heavy rain and snow in October in especially
eastern Greenland gave record totals of precipitation in the main east
coast town of Tasiilaq as the remnants of former hurricane Nicole
passed by and, much as with Harvey in Houston this year, got lodged
over eastern Greenland for some days. However, after Nicole's
extreme precipitation, the rest of the winter was actually pretty
average in terms of the amount of snow that fell, and indeed parts of
north western Greenland had less snow than usual, as can be seen in
the accumulated SMB anomaly map below.
The other important process this year has been a relatively
short and below average melt and runoff season. The summer melt
season is extremely important for the annual SMB and the overall
health of the ice sheet. The date of onset of the melt season
was the 3rd earliest on record but it was then followed by a cold and
snowy period so that the onset of high rates of ice loss (more than
1Gt of ice lost per day, known as the ablation season) was actually
average. Going into summer with a large amount of accumulated
fresh snow means that the albedo feedback took longer to kick in.
Albedo, the reflectivity of the surface, is a very important control
on the rate of melt of glacier ice. Fresh snow is bright and
reflective and slower to melt, but when the older and darker snow and
glacier ice is exposed underneath, surface melt accelerates. The large
amount of fresh snow in June substantially dampened this
feedback.
(CLIP....)