The National Snow and Ice Data Center (NSIDC) is part of the Cooperative Institute for Research in Environmental Sciences at the University of Colorado Boulder. NSIDC scientists provide Arctic Sea Ice News & Analysis content, with partial support from NASA.
Unusually high air temperatures and a warm ocean have led to a record low Arctic sea ice extent for November, according to scientists at the National Snow and Ice Data Center (NSIDC). In the Southern Hemisphere, Antarctic sea ice extent also hit a record low for the month, caused by moderately warm temperatures and a rapid shift in circumpolar winds.
Arctic sea ice extent averaged 9.08 million square kilometers (3.51 million square miles) for November, 1.95 million square kilometers (753,000 square miles) below the 1981 to 2010 long-term average for the month. Although the rate of Arctic ice growth was slightly faster than average, total extent actually decreased for a brief period in the middle of the month. The decrease in extent measured 50,000 square kilometers (19,300 square miles) and was observed mostly in the Barents Sea, an area of the Arctic Ocean north of Norway, Finland, and Eastern Russia. NSIDC scientists said the decrease in extent is almost unprecedented for November in the satellite record; a less pronounced and brief retreat of 14,000 square kilometers (5,400 square miles) happened in 2013.
November 2016 is now the seventh month this year to have hit a record low extent in the 38-year satellite monitoring period. The November extent was 3.2 standard deviations below the long-term average, a larger departure than observed in September 2012 when the Arctic summer minimum extent hit a record low.
Arctic sea ice is still in the early stages of winter freeze-up and is expected to continue expanding until it hits its maximum extent around March next year.
NSIDC scientists said unusually high temperatures over the Arctic Ocean, persistent winds from the south, and a warm ocean worked together to drive the record low Arctic extent. Extending from northeast of Greenland towards Svalbard and Severnaya Zemlya, air temperatures at the 925 hPa level (about 2,500 feet above sea level) were up to 10 degrees Celsius (18 degrees Fahrenheit) above the 1981 to 2010 long-term average for the month. Sea surface temperatures in the Barents and Kara Seas remained unusually high, up to 4 degrees Celsius (7 degrees Fahrenheit) above average around Novaya Zemlya and Svalbard, preventing ice formation. These high temperatures reflected a pattern of winds from the south, which also helped to push the ice northward and reduce the ice extent.
NSIDC scientist Julienne Stroeve was in Svalbard during November and noted the lack of sea ice. “Typically sea ice begins to form in the fjords at the beginning of November, but this year there was no ice to be found,” she said.
“It looks like a triple whammy—a warm ocean, a warm atmosphere, and a wind pattern all working against the ice in the Arctic,” said NSIDC director Mark Serreze.
In the Southern Hemisphere, sea ice surrounding the continent of Antarctica declined very quickly early in the month, and remained far below the range of past November daily extents. The average extent for the month of November was 14.54 million square kilometers (5.61 million square miles), 1.81 million square kilometers (699,000 square miles) below the 1981 to 2010 average. This was more than twice the previous record departure from average set in November 1986 and was 5.7 standard deviations below the long-term average.
NSIDC scientists said that higher than average air temperatures and a rapid shift in Antarctic circumpolar winds appears to have caused the rapid decline in Antarctic sea ice.
Air temperatures 2 to 4 degrees Celsius, or 4 to 7 degrees Fahrenheit higher than average and an earlier pattern of strong westerly winds worked to create a more dispersed sea ice pack in the Antarctic. A rapid shift to a more varied wind structure, with three major areas of winds from the north, rapidly compressed low-concentration sea ice around Wilkes Land, Dronning Maud Land, Enderby Land, and the Antarctic Peninsula. Moreover, several very large polynyas (areas of open water within the pack) have opened in the eastern Weddell and along the Amundsen Sea and Ross Sea coasts.
NSIDC lead scientist Ted Scambos said, “Antarctic sea ice really went down the rabbit hole this time. There are a few things we can say about what happened, but we need to look deeper.”
NASA scientist and NSIDC affiliate scientist Walt Meier said, “The Arctic has typically been where the most interest lies, but this month, the Antarctic has flipped the script and it is southern sea ice that is surprising us.”
See the full analysis and relevant graphs and images in the NSIDC Arctic Sea Ice News & Analysis page.
See the NASA Earth Observatory feature.
See the Climate.gov feature.
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