What continues to be unclear is
the gross mass of new ice produced. An
inch of extra thickness could make a vast difference. We never really know and gross area is a
serious misdirection.
As I have posted in the past,
there is ample reason to think that a pretty stable surplus deltaH of warmer
water is injected into the arctic every year and has been done for at least
fifty years. At least it provides us a
sound explanation for what has been seen.
If the deltaH has been applied over sixty years, then the amount of
deltaH is a lot smaller that if the effect was applied only recently and this
is supported by the slow erosion observed.
It also suggests that a reversal is a fairly small event and also may go
unnoticed. Just how much does the key
ocean current need to alter to do the job?
Otherwise, the present warm spell
in the high Arctic is continuing and will do so until further notice.
Arctic sea ice extent below average in March: data center
2012's sea ice stayed around longer, but it's likely to melt
quickly
April 05, 2012 - 9:28 am
Arctic sea ice extent in March
2012 averaged 15.21 million square kilometres. The magenta line shows the 1979
to 2000 median extent for that month. The black cross indicates the geographic
North Pole. (IMAGE COURTESY OF THE NSIDC)
NUNATSIAQ NEWS
Arctic sea ice extent in March
2012 averaged 15.21 million square kilometres. The magenta line shows the 1979
to 2000 median extent for that month. The black cross indicates the geographic
North Pole. (IMAGE COURTESY OF THE NSIDC)
You may not be able to note
the changes when you look out the window and still see frozen sea ice, but
Arctic sea ice has already entered the spring melt season.
Arctic sea ice reached its
annual maximum extent on March 18, says the Colorado-based National Snow and
Ice Data Center, which uses satellite data to see how much of the Arctic Ocean
sea ice covers.
Now the sea ice has started to
shrink.
And while sea ice extent for
March as a whole was higher than in recent years, it still came in below
average, the NSIDC said in an April 4 update on sea ice conditions in the
Arctic.
Arctic sea ice extent this
March ranked in the bottom ten recorded over the past 34 years of satellite
data, coming in ninth lowest.
Over that 34-year period,
the day of the maximum sea ice extent has varied by more than six weeks,
occurring as early as mid-February and as late as the end of March.
However, even with so much
variability, the NSIDC says there is a “small trend” towards maximum sea ice
extents occurring later.
This year’s maximum sea ice
extent continued that trend, occurring on March 18, 12 days later than average,
the NSIDC said.
It’s not clear why the maximum
sea ice extent would happen later, given that, in general, Arctic sea ice
extent is decreasing, it noted.
One possibility is that the
lower winter sea ice extents might make it easier for ice to continue growing
later in the season, or that a late cold snap or northerly winds could spread
ice southward over parts of the ocean that would normally be ice-covered at
that point.
But the new sea ice growth is
very thin and likely to melt quickly, the NSIDC said.
That’s because sea ice age
data shows that winter sea ice continues to be dominated by younger and thinner
sea ice.
So, researchers do not expect
the late maximum sea ice extent to strongly influence summer melt.
“The ice that grew late this
winter is quite thin, and will melt rapidly as the sun rises higher in the sky
and the air and water get warmer,” the NSIDC said.
No comments:
Post a Comment