From the National Snow & Ice Data Center:
After a period of slow ice loss in the middle of June, Arctic sea ice loss ramped up, and extent at the end of the month fell below 2012, the year which ended up with the lowest September ice extent in the satellite record. A pattern of atmospheric circulation favored ice loss this June, which was also characterized by above average temperatures over most of the Arctic Ocean, and especially in the Laptev and East Siberian Seas.
Overview of conditions
Arctic sea ice extent for June averaged 10.53 million square kilometers (4.07 million square miles). This is 1.23 million square kilometers (475,000 square miles) below the 1981 to 2010 average and 120,000 square kilometers (46,300 square miles) above the previous June record low set in 2016. Extent at the end of the month remained well below average on the Pacific side of the Arctic, with open water extending from the Bering Strait, and along the coasts of the Chukchi and Beaufort Seas all the way to Melville Island in the Canadian Arctic Archipelago. Sea surface temperatures (SSTs) in the open waters have been unusually high, up to 5 degrees Celsius (9 degrees Fahrenheit) above average in the Chukchi Sea, as indicated by the National Oceanic and Atmospheric Administration (NOAA) SST data provided on the University of Washington Polar Science Center UpTempO website. Large areas of open water are now apparent in the Laptev and Kara Seas with extent below average in Baffin Bay and along the southeast coast of Greenland.
Extent over the first 10 days of the month dropped quickly but then the loss rate suddenly slowed. From June 12 through June 16, extent remained almost constant at 10.8 million square kilometers (4.17 million square miles). Following this hiatus, extent then dropped fairly quickly through the remainder of the month. Overall, sea ice retreated almost everywhere in the Arctic in June. Exceptions included the northern East Greenland Sea, southeast of Svalbard, near Franz Joseph Land, and in the southeastern part of the Beaufort Sea, where the ice edge expanded slightly.
Conditions in context
Following May’s theme, air temperatures at the 925 hPa level (about 2,500 feet above the surface) in June were above the 1981 to 2010 average over most of the Arctic Ocean. However, the spatial patterns between the two months were different. While in May, it was particularly warm compared to average over Baffin Bay and a broad area north of Greenland, in June the maximum warmth of more than 6 to 8 degrees Celsius (11 to 14 degrees Fahrenheit) shifted to the Laptev and East Siberian Seas (Figure 2b). It was slightly cooler than average over the northern Barents and Kara Seas and over central Greenland and the western Canadian Arctic.
The atmospheric circulation at sea level featured high pressure over the north American side of the Arctic, with pressure maxima over Greenland and in the Beaufort Sea, paired with low pressure over the Eurasian side of the Arctic, with the lowest pressures over the Kara Sea (Figure 2c). This pattern drew in warm air from the south over the Laptev Sea where temperatures were especially high relative to average. This circulation pattern bears some resemblance to the Arctic Dipole pattern that is known to favor summer sea ice loss, which was particularly well developed through the summer of 2007. So far, the pattern for the 2019 melt season is very different than the past three years, which featured low pressure over the central Arctic Ocean.
June 2019 compared to previous years
The average extent for June 2019 of 10.53 million square kilometers (4.07 million square miles) ended up as the second lowest in the satellite record. The current record low of 10.41 million square kilometers (4.02 million square miles) was set in June 2016. Overall, sea ice extent during June 2019 decreased by 2.03 million square kilometers (784,00 square miles). Because of the fairly slow loss rate near the middle of the month, the overall loss rate for June ended up being fairly close to the 1981 to 2010 average. The linear rate of sea ice decline for June from 1979 to 2019 is 48,000 square kilometers (19,00 square miles) per year, or 4.08 percent per decade relative to the 1981 to 2010 average.
Sea Ice Outlook posted for June
The Sea Ice Prediction Network–Phase 2 recently posted the 2019 Sea Ice Outlook June report. This report focuses on projections of September sea ice extent based on conditions in May. The projections come variously from complex numerical models to statistical models to qualitative perspectives from citizen scientists. There were 31 contributions for projected total Arctic sea ice extent and of these 31, nine also provided projections for extent in Alaska waters, and six provided projections of total Antarctic extent (Figure 4). There were also seven predictions of September extent for Hudson Bay.
The median of the projections for the monthly mean September 2019 total Arctic sea ice sea-ice extent is 4.40 million square kilometers (1.70 million square miles) with quartiles (including 75 percent of the 31 projections) of 4.2 and 4.8 million square kilometers (1.62 and 1.85 million square miles). The observed record low September extent of 3.6 million square kilometers (1.39 million square miles) was set 2012. Only three of the projections are for a September 2019 extent below 4.0 million square kilometers (1.54 million square miles) and only one is for a new record at 3.06 million square kilometers (1.18 million square miles).
Thicker clouds accelerate sea decline
A new study led by Yiyi Huang of the University of Arizona presents evidence of a link between springtime cloud cover (Figure 5) over the Arctic Ocean and the observed decline in sea ice extent. Based on a combination of observations and model experiments, there may be a reinforcing feedback loop. As sea ice melts, there is more open water which promotes more evaporation from the surface and hence more water vapor in the atmosphere. More water vapor in the air then promotes the development of more clouds. This increases the emission of longwave radiation to the surface, further fostering melt. The process appears to be effective from April through June. But since the atmosphere influences the sea ice and the sea ice influences the atmosphere, separating cause and effect remains unclear.
Antarctic sea ice at record low for June
Sea ice surrounding Antarctica was at the lowest mean monthly extent for June, surpassing 2002 and 2017. At the month’s end, sea ice averaged approximately 160,000 square kilometers (62,000 square miles) below the previous record low set in 2002, and over 1.1 million square kilometers (425,000 square miles) below the 1981 to 2010 average. Ice extent was particularly low in the eastern Weddell Sea and the region north of Enderby Land (south of the western Indian Ocean), and north of eastern Wilkes Land. No region had substantially above average sea ice extent in June.
A new paper published by our colleague Claire Parkinson at NASA Goddard Space Flight Center (GSFC) discusses the large drop in Antarctic sea ice extent between 2014 and 2017. The winter maximum for 2014 was unusually high, setting the 40-year record maximum extent. Our earlier posts noted the dramatic recent decline, particularly in the austral spring of 2016. Sea ice has remained below the 1981 to 2010 reference period extent since late 2016.
While the recent decline is noteworthy, trends in Antarctic sea ice extent over the continuous satellite record since late 1978 remain slightly positive (Figure 6a). Antarctica experiences large inter-annual variability because of its unconfined geography—open to the Southern Ocean on all sides—and strong influences of the varying Southern Annular Mode pattern of atmospheric circulation. Sparse satellite data from the 1960s indicate large swings in that decade as well. Previous studies have attributed the onset of the recent decline as a response to a series of intense storms. Unlike Arctic sea ice extent, which evinces a longterm downward trend, Antarctic sea ice extent displays enormous variability that is natural for the southern sea ice system (Figure 6b). Thus, a clear climate-related signal cannot yet be discerned for sea ice in the southern hemisphere.