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Open water means a warm Arctic


Autumn over the Arctic Ocean is a season of falling temperatures and rapid growth of sea ice. However, as in recent years, low sea ice extent at the beginning of autumn means large transfers of heat to the atmosphere from open water areas, keeping the Arctic warmer than usual. Despite this warmth, freeze up is in high gear.

Overview of conditions

Figure 1. Arctic sea ice extent for October 15, 2012 was 5.18 million square kilometers (2.00 million square miles). The orange line shows the 1979 to 2000 median extent for that day. The black cross indicates the geographic North Pole. Sea Ice Index data. About the data

Credit: National Snow and Ice Data Center
High-resolution image

As of October 15, sea ice extent stood at 5.18 million square kilometers (2.00 million square miles). This is 3.49 million square kilometers (1.35 million square miles) below the 1979 to 2000 mean for this time of year and 70,000 square kilometers (27,000 square miles) below the same date in 2007. Although it is still at record low levels, extent is climbing fast.

Large areas of the Kara, Laptev, East Siberian, Chukchi, and Beaufort seas remain open for hundreds of kilometers offshore. East of Greenland, ice extent is near average.

Conditions in context

Figure 2. The graph above shows Arctic sea ice extent as of October 15, 2012, along with daily ice extent data for the previous five years. 2012 is shown in blue, 2011 in orange, 2010 in pink, 2009 in navy, 2008 in purple, and 2007 in green. The gray area around the average line shows the two standard deviation range of the data. Sea Ice Index data.

Credit: National Snow and Ice Data Center
High-resolution image

Arctic sea ice extent is increasing rapidly, at about 100,000 square kilometers (38,600 square miles) per day, expanding southward at the ice edge, as well as northward from the Arctic continental coasts. However, sea ice extent is still at record low levels for the date, compared to the satellite measurement period (1979 to 2012). On October 6, daily sea ice extent climbed above the 2007 record daily minimum (4.17 million square kilometers or 1.61 million square miles), having spent forty days below that level. On October 14, extent went above 5.0 million square kilometers (1.93 million square miles) for the first time since mid-August.

Open water warms the lower atmosphere

Figure 3. This figure shows air temperatures as a function of height and longitude at 75 degrees north latitude. Temperatures are for the period September 20 to October 10, 2012 compared to averages for the years 1981 to 2010. Between longitudes 120 degrees west to 150 degrees west, temperatures more than 4 degrees Celsius (7 degrees Fahrenheit) above normal are found up to the 850 hPa level (roughly 4500 feet above the surface), with temperatures near the surface, in closer proximity to the warming effects of the ocean, more than 6 degrees Celsius (11 degrees Fahrenheit) above normal.

Credit: NSIDC courtesy NOAA/ESRL PSD
High-resolution image

The past decade has seen much stronger increases in air temperature in the Arctic compared to the globe as a whole. While this strong warming, known as Arctic amplification, has a number of causes, a primary one is declining summer sea ice extent. Through summer, solar energy is readily absorbed within expanding areas of dark, open water. When the sun sets, this heat stored in the uppermost layers of the Arctic Ocean is released upwards, keeping the overlying atmosphere unusually warm.

This warming effect has been especially pronounced during the early autumn of 2012. Air temperatures averaged over the most recent thirty days of data are above average over nearly all of the Arctic Ocean. The warmest conditions compared to average are over northwestern Canada and extending into the Beaufort Sea. Here, the effect of heat released from the ocean is augmented by warm, southerly winds, and is linked to a pattern of unusually high pressure centered over the Gulf of Alaska.

Arctic wind patterns support melting, ice export

Figure 4. Sea level pressure for June 2007 to 2012 compared to averages over the period 1981 to 2010. The Arctic dipole anomaly refers to the combination of unusually high pressure over the northern Beaufort Sea and Greenland and unusually low pressure over northern Eurasia.

Credit: NSIDC courtesy NOAA/ESRL PSD
High-resolution image

Recent research led by James Overland of the National Oceanic and Atmospheric Administration (NOAA) and Jennifer Francis of Rutgers University shows that the Arctic dipole anomaly, featuring unusually high pressure over the northern Beaufort Sea and Greenland and unusually low pressure over northeastern Eurasia, has become more common in the early summer of recent years.

As discussed in previous posts, this pattern brings in warm southerly winds along the shores of the East Siberian and Chukchi seas. It favors strong ice melt in these sectors and pushes the ice away from the coast, leaving open water. The pressure pattern also favors the transport of ice out of the Arctic Ocean and into the North Atlantic through Fram Strait.

The Arctic dipole anomaly was very well developed throughout the summer of 2007 and was in part responsible for the very low September ice extent recorded that year (the second lowest in the satellite record). According to Overland and colleagues, no other six-year period matches the intensity and persistence of the June pattern for 2007 to 2012 in the past sixty-three years. The pattern is linked to the general weakening of the circumpolar jet stream and the greater meandering of this wind flow.

Recall from our previous post that the summer of 2012 as a whole saw a somewhat different pattern. Unusually low pressure was present along the Eurasian coastal seas and extended eastward into the Beaufort Sea, most prominently over the East Siberian Sea, with unusually high pressure centered over Greenland and the northern North Atlantic.

Antarctic sea ice extent remains above average

Figure 5. This graph shows the highest extent years for Antarctic sea ice. The blue line shows 2012, the orange line shows 2011, the green line shows 2007, and the pink line shows 2006. The 1979 to 2000 average is in dark gray. The gray area around this average line shows the two standard deviation range of the data. Sea Ice Index data.

Credit: National Snow and Ice Data Center
High-resolution image

Antarctic sea ice extent dropped below record levels seen for the date but remains well above average. Journalists inquired about the cause of gradual growth in wintertime Antarctic sea ice and the record high Antarctic sea ice extent in mid-September despite general climate warming and the dramatic sea ice losses in the Arctic. As we noted in the previous post, researchers cite stronger westerly winds surrounding Antarctica, in contrast to the Arctic. See also the following news stories on Antarctic sea ice, to which NSIDC scientists contributed, under “Further reading” below.

Further reading

Peter Aldhous, “Why sea ice records are poles apart,” New Scientist, October 8, 2012.

Justin Gillis, “Running the numbers on Antarctic sea ice,” New York Times Green blog, October 3, 2012.

Richard Harris, “Scientists watch Antarctica, Arctic sea ice levels,” National Public Radio Morning Edition, October 8, 2012.


Overland, J. E., J. A. Francis, E. Hanna, and M. Wang. 2012. The recent shift in early summer Arctic atmospheric circulation. Geophysical Research Letters 39, L19804, doi: 10.1029/2012GL053268.


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