Some mixed news from the National
Snow and Ice Data Center (NSIDC) provides us with a preliminary update on the
Arctic sea ice conditions for the winter of 2013 and a foreshadowing of what the summer might bring to the Arctic.
Scientists at NSIDC estimate that the Arctic sea ice reached its
maximum extent on March 15, 2013, the date that marks the beginning of the 2013
ice melting season. The maximum areal extent reached 5.84 million square
miles or 15.13 million square kilometres, 283,000 square miles or 733,000
square kilometres below the 1979 to 2000 average areal extent. This is
the sixth lowest maximum sea ice extent since the satellite record began.
It also continues a streak of the 10 lowest maximums all of which have occurred in the last 10 years.
Here is a map and a graph showing the Arctic
ice extent this winter and the areal extent over the past five winter seasons and the average for the period
from 1979 to 2000:
This past winter, Arctic sea ice
extent grew by a record 4.53 million square miles or 11.72 million square
kilometres. Before we pat ourselves on the back, here's what happened
last summer:
On September 16, 2012, Arctic sea
ice reached its minimum extent of 1.32 million square miles or 3.41 million
square kilometres, the lowest seasonal minimum sea ice extent in the satellite
record which goes back to 1979. This was 1.32 million square miles or
3.43 million square kilometres below the average between 1979 and 2000.
The larger than normal areal extent of open water forms a feedback into
the environment; more open water means that there are larger transfers of heat
from the open water areas to the atmosphere which keeps the entire Arctic ecosystem
warmer than usual.
Here is a similar graphic to the one
shown above, showing the Arctic ice extent over the past five summer seasons
and the average for the period between 1979 and 2000:
As I noted above, during the
freezing season of 2012 - 2013, the areal extent of sea ice grew by a record
amount, surpassing the old record by 5.5 percent. Unfortunately, all of
this ice is classified as "first-year ice". Multi-year ice which has been through several freeze-thaw cycles contains much less brine and
more air pockets than first year ice. It is stiffer and is much more
resistant to melting than first-year ice. If first-year ice does not grow
thick enough over the winter period, it will completely melt during the
following summer.
Here is a video from NASA showing how the areal extent of multi-year Arctic sea ice has declined over the past three decades:
It will be interesting to see how
next summer's Arctic ice situation measures up when compared to other years.
With a record low areal ice extent this winter and formation of vast
areas of fragile first-year ice, the globe could once again find itself breaking
last year's minimum Arctic ice extent record.
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