Steven Goddard writes below that he agrees with the prediction I made in late 2009 that we’d see another 500,000 km2 of Arctic sea ice recovery in 2010. The Arctic Oscillation seems to be negative again, and according to NSIDC, this figures greatly in making thicker ice thus lowering summer losses. – Anthony

Source: Climate Prediction Center

NSIDC regularly puts out a news article describing the deteriorating state of the Arctic, called the Sea Ice News. In their May 5, 2008 article, they stated:

…the Arctic Oscillation was in its positive phase through the winter season, associated with a wind pattern helping to flush thick ice out of the Arctic, leaving thinner ice. This is one of the factors helping to set the stage for pronounced ice losses this summer.

Additionally, Dr. Walt Meier from NSIDC told WUWT:

The NAO/AO (Arctic Oscillation) is a particularly prominent one and a substantial amount of the decline in the sea ice during the late 1980s and early 1990s could be attributed to a strong positive mode during winters because the positive mode favors the loss of thicker ice (through drift) that is less likely to melt during summer.

In their January 5, 2010 article NSIDC states that we are in an “Extreme negative phase of the Arctic Oscillation” which can be seen in this NOAA graph below. Oddly (but not surprisingly) the article failed to mention how this affects drift.

If a positive Arctic Oscillation flushes out the Arctic into the Atlantic, the implication is that a negative phase would tend to retain ice. This indeed appears to be the case. Arctic buoys show very light polar drift this winter.

NSIDC made a big deal about loss of multi-year ice in the Arctic during 2007-2008, but this was due more to drift in the winter than melting in the summer, as can be seen in the NSIDC map pair below. Note that most of the 2007 multiyear ice was replaced by first year ice after the 2007 melt season ended and (necessarily) before the 2008 melt season started. The only way this could have happened was due to drift during the 2007-2008 winter, i.e. it could not be the result of summer melt -because ice only forms in the winter.

If the ice is not drifting (i.e. not under tensile stress) the concentration should be high. This indeed appears to be the case. According to UIUC maps, sea ice concentration is high (above 90%) across the Arctic Basin.

http://arctic.atmos.uiuc.edu/cryosphere/NEWIMAGES/arctic.seaice.color.000.png

The Arctic ice minimum extent increased by about 25% between 2007 and 2009, and many indications (negative AO, light drift, high concentration) point to the idea that it will continue to increase in 2010.

http://www.ijis.iarc.uaf.edu/seaice/extent/AMSRE_Sea_Ice_Extent.png

We can also expect that the average age of the ice has increased this winter, continuing a trend started in 2009.

Here’s your chance to weigh in:

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