Arctic Sea Ice Collapse Threatens - Update 6
24
August, 2015
The
image below shows Arctic sea ice extent, with the blue dot
indicating that extent for August 22, 2015, was 5.382 million square
kilometers. The record shows that, at this time of the year, extent
was only lower in 2007, 2011 and 2012.
There are a number of reasons why sea ice could fall dramatically over the next few weeks.
First
of all, the situation today is in an even worse condition than one
might conclude when looking at sea ice extent alone. The way NSIDC
calculates extent is by first dividing the satellite image into a
grid and then including each cell in extent that has 15% or more
ice. So, if a few small and very thin pieces of ice floating in a
cell happen to cover 15% of a cell, it is counted in as "sea
ice".
There is quite a difference between the sea ice that was 5 meters thick north of Greenland in 2012 and the ice that is present there now. The image on the right shows the north-east corner of Greenland on the bottom left. There is almost no ice north of this point.
Thick sea ice is virtually absent compared to the situation in the year 2012 around this time of year, as illustrated by the image below that compares sea ice thickness on August 20, 2012 (left) with August 20, 2015 (right), from an earlier post.
There is quite a difference between the sea ice that was 5 meters thick north of Greenland in 2012 and the ice that is present there now. The image on the right shows the north-east corner of Greenland on the bottom left. There is almost no ice north of this point.
Thick sea ice is virtually absent compared to the situation in the year 2012 around this time of year, as illustrated by the image below that compares sea ice thickness on August 20, 2012 (left) with August 20, 2015 (right), from an earlier post.
Furthermore,
sea surface temperatures are very high. The North Pacific, on August
23, 2015, was exactly 1°C (1.8°F) warmer than it was compared to
the period from 1971 to 2000 (see Climate
Reanalyzer image
right).
As the image below shows, sea surface temperature anomalies are very high around North America. On August 23, 2015, sea surface temperature anomalies as high as 6.4°C (11.5°F) were recorded in the Bering Strait.
This is where warm waters from the Pacific Ocean are flowing into the Arctic Ocean.
As the image below shows, sea surface temperature anomalies are very high around North America. On August 23, 2015, sea surface temperature anomalies as high as 6.4°C (11.5°F) were recorded in the Bering Strait.
This is where warm waters from the Pacific Ocean are flowing into the Arctic Ocean.
The image below shows sea surface temperatures on August 22, 2015, indicating that a huge amount of ocean heat has accumulated in the Atlantic Ocean off the coast of North America.
The Gulf Stream is carrying much of this warm water toward the Arctic Ocean. On August 21, 2015, sea surface temperatures near Svalbard were as high as 17°C (62.6°F), a 12°C (21.5°F) anomaly, at the location marked by the green circle on the image below, showing sea surface temperatures in the top panel and sea surface temperature anomalies in the bottom panel.
The
image below shows sea surface temperature anomalies in the Arctic as
at August 23, 2015.
[
click on image to enlarge ]
|
There
still are a few weeks to go before sea ice can be expected to reach
its minimum, at around half September 2015, while sea currents will
continue to carry warmer water into the Arctic Ocean for months to
come.
More open water increases the chance that storms will develop that will push the last remnants of the sea ice out of the Arctic Ocean, as discussed in earlier posts such as this one, while storms can also mix warm surface waters all the way down to the seafloor, as discussed inthis earlier post. The Climate Reanalyzer forecast for August 26, 2015, on the right shows strong winds both in the Bering Strait and the North Atlantic.
Typhoons increase this danger. The Climate Reanalyzer forecast for August 27, 2015, below shows a typhoon in the Pacific Ocean close to the Arctic Ocean.
More open water increases the chance that storms will develop that will push the last remnants of the sea ice out of the Arctic Ocean, as discussed in earlier posts such as this one, while storms can also mix warm surface waters all the way down to the seafloor, as discussed inthis earlier post. The Climate Reanalyzer forecast for August 26, 2015, on the right shows strong winds both in the Bering Strait and the North Atlantic.
Typhoons increase this danger. The Climate Reanalyzer forecast for August 27, 2015, below shows a typhoon in the Pacific Ocean close to the Arctic Ocean.
The situation is dire and calls for comprehensive and effective action, as discussed in the Climate Plan.
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