Press releases

Low sea-ice cover in the Arctic

Second-lowest September minimum since observations
Diese Aufnahme stammt aus der IceCam des EM-Birds, einem Meereisdickensensor, der unter einem Hubschrauber hängend über das Meereis geflogen wird. Die Kamera ist derart in das Geräte eingebaut, dass sie immer senkrecht in die Tiefe fotografiert.

This image was taken with the IceCam, installed in the hull of the EM-Bird, the AWI sea ice thickness measuring sensor, which in pulled underneath a helicopter above the sea ice to measure its thickness. The camera points vertically downwards and takes photos of the area directly underneath the bird.
IceCam Arctic sea ice (Photo: Alfred Wegener Institute / IceCam/Stefan Hendricks)

The sea-ice extent in the Arctic is nearing its annual minimum at the end of the melt season in September. Only circa 3.9 million square kilometres of the Arctic Ocean are covered by sea ice any more, according to researchers from the Alfred Wegener Institute and the University of Bremen. This is only the second time that the annual minimum has dropped below four million square kilometres since satellite measurements began in 1979.

Common press release: Alfred Wegener Institute and Bremen University

Until mid-August, it looked as though a notable record would be reached: the area of the Arctic Ocean covered by ice (defined as the area with a sea-ice concentration of more than 15 percent) from late March to early August was the smallest measured by satellites since 1979.

“Our satellite data show that between March and April 2019, there was an unusually large decrease in the ice extent, from which the Arctic sea ice was unable to recover,” explain Prof. Christian Haas, a geophysicist and head of the Sea Ice section at the Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research (AWI) and Dr Gunnar Spreen from the University of Bremen’s Institute for Environmental Physics. Since the second half of August, however, the seasonal reduction has slowed down, overlaid by short-term fluctuations. The lowest value so far for 2019 was 3.82 Million square kilometres, observed on 3 September. This means that this year, the September average could be below 4 million square kilometres for only the second time.

But in the coming weeks, the ice could retreat further: even though in early fall air temperatures in the Arctic have now fallen below freezing, the heat stored in the water can continue to melt the underside of the ice for a few more weeks. However, if it becomes extremely cold in the Arctic in the days ahead, the ice cover can already increase again. In October, the scientists will analyse the data for the whole of September, and will then be able to make a final assessment of the sea-ice minimum in 2019. It appears unlikely that this year we will see a new absolute record, below the sea-ice extent of 3.4 million square kilometres observed in 2012. “Record or not, this year confirms the continued long-term reduction of Arctic sea ice as a result of climate change, making it ever more likely that in a few decades the Arctic will be ice free in summer. This will mean drastic changes in the Arctic, with consequences for the climate and ecosystems, as well as for people, including us in Europe,” says Christian Haas.

Scientists at the Alfred Wegener Institute and the Institute for Environmental Physics at the University of Bremen are together analysing the complete satellite data on the ice concentration, extent, and thickness, as well as atmospheric measurements. The meereisportal.de , for example, publishes daily updated ice maps and provides detailed summaries of the sea-ice developments. Ice extent estimates from other institutions (e.g. NSIDC or OSI-SAF) can provide slightly different results. Currently, for 2019 they predict the third-lowest ice extent. “These slight differences are due to the higher resolution of our data and the slightly different methods used to calculate the ice concentration. They show the uncertainties that even the most modern satellite observations can have. Data from the MOSAiC expedition will help to reduce these uncertainties,” explains Dr Gunnar Spreen from the University of Bremen’s Institute for Environmental Physics.

The researchers are currently particularly interested in the northern Laptev Sea: on 20 September, the research icebreaker Polarstern will set sail from Tromsø, in Norway, for the start of the MOSAiC expedition. In the northern Laptev Sea they will search for a suitable ice floe to moor the Polarstern to, in order to drift, icebound, through the Central Arctic for an entire year. “We’re following the ice situation very closely and have developed a series of new data products to offer the best-possible, detailed insights into the current conditions,” reports Christian Haas. “In the Laptev Sea, the ice situation is similar to previous years with an Arctic-wide low ice extent. This means that it will be relatively easy for us to reach our research area, at a latitude of 85 degrees north. But being so close to the ice edge will make it difficult to find a suitable ice floe that is large enough and thick enough to set up our ice camp. Our computer models show that the ice south of 88 degrees north is less than 80 centimetres thick, which is less than the 1.2 metres we’d ideally like to have to safely set up our measuring stations. We may have to travel farther north than planned to find the right conditions,” expects Christian Haas, who will lead the second leg of the MOSAiC expedition from mid-December.

More detailed information is given in the meereisportal.de.

Contact

Science

Christian Haas
+49(471)4831-2285

Press Office

Folke Mehrtens
+49(0)471 4831-2007

Universität Bremen

Wissenschaft
Gunnar Spreen
University of Bremen - Institute of Environmental Physics
+49-421-218-62158
gunnar.spreen@uni-bremen.de

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Diese Aufnahme stammt aus der IceCam des EM-Birds, einem Meereisdickensensor, der unter einem Hubschrauber hängend über das Meereis geflogen wird. Die Kamera ist derart in das Geräte eingebaut, dass sie immer senkrecht in die Tiefe fotografiert.

This image was taken with the IceCam, installed in the hull of the EM-Bird, the AWI sea ice thickness measuring sensor, which in pulled underneath a helicopter above the sea ice to measure its thickness. The camera points vertically downwards and takes photos of the area directly underneath the bird.
This image was taken with the IceCam, installed in the hull of the EM-Bird, the AWI sea ice thickness measuring sensor, which in pulled underneath a helicopter above the sea ice to measure its thickness. The camera points vertically downwards and takes photos of the are... (Photo: Alfred Wegener Institute / IceCam/Stefan Hendricks)
Karte der Meereisausdehnung am 11. September 2019. Zum Vergleich sind in minimalen Eisausdehnungen 2007 (Rot) und 2012 (Gelb) gezeigt. In beiden Jahren wurden wir die bisher niedrigsten Meereisausdehnungen erreicht. Ergänzend ist die mögliche MOSAiC Startregion in schwarz gekennzeichnet.
Map of the Arctic sea ice extend on 11 September 2019. For comparison, the minimum extend in 2007 (red line) and 2012 (yellow line) are displayed, the years with the lowest summer minima to date. Additionally, the starting region for the MOSAiC expedition with RV Polars... (Graphic: Alfred Wegener Institute / meereisportal.de)
Monatsmittelwerte der Meereisausdehnung im September in der Arktis seit 1979. In Rot der vorraussichtliche Wert für September 2019 +/- zweifache Standardabweichung
Monthly mean of September sea ice extend from 1979 to 2019. The estimated value (+/- two standard deviations) is given in red. (Graphic: Alfred-Wegener-Institut)
Tägliche Meereisausdehnung in der Arktis bis zum 11. September 2019 (rot). Zum Vergleich ist die Ausdehnung von 2018, 2017, 2016, 2012 und 2007 dargestellt, sowie das Langzeitmittel von 1981-2010 (grau) mit dem Bereich von zwei Standardabweichungen (hellgrau).
Daily Arctic sea ice extend including 11September for 2019 (red line). For comparison: the extend for the years 2018, 2017, 2016, 2012, 2007 and the long-term mean from 1981 to 2010 (grey line) and the area of two standard deviation from it (light grey). (Graphic: Alfred-Wegener-Institut)
Der deutsche Forschungseisbrecher Polarstern treibt für Forschungsarbeiten über dem Bereich der 'Aurora' Hydrothermalquellen am Westlichen Gakkel Rücken bei ca. 82¡53'N und 6¡15'W.

Foto von der Polarstern-Arktis-Expedition AURORA (PS86); Sie war der Untersuchung von geophysikalischen, geologischen, geochemischen und biologischen Prozessen an Hydrothermalquellen des Gakkelrückens gewidmet.
The Germa Research Icebreaker Polarstern in the Arctic (Photo: Alfred Wegener Institute / Stefanie Arndt)
Arctic, August 2012: Aerial photo of Arctic sea ice in the record year 2012.  Photo: NADIR/Stefan Hendricks, Alfred-Wegener-Institut

Arktis, August 2012: Luftaufnahme von arktischem Meereis im Negativrekordjahr 2012. Foto: NADIR/Stefan Hendricks, Alfred-Wegener-Institut
Arctic, August 2012: Aerial photo of Arctic sea ice in the record year 2012. (Photo: Alfred Wegener Institute / Stefan Hendricks / NADIR)
Junges Arktisches Meereis.

Diese Aufnahme stammt aus der IceCam des EM-Birds, einem Meereisdickensensor, der unter einem Hubschrauber hängend über das Meereis geflogen wird. Die Kamera ist derart in das Geräte eingebaut, dass sie immer senkrecht in die Tiefe fotografiert.

engl.

Young Arctic sea ice.


This image was taken with the IceCam, installed in the hull of the EM-Bird, the AWI sea ice thickness measuring sensor, which in pulled underneath a helicopter above the sea ice to measure its thickness. The camera points vertically downwards and takes photos of the area directly underneath the bird.
This image was taken with the IceCam, installed in the hull of the EM-Bird, the AWI sea ice thickness measuring sensor, which in pulled underneath a helicopter above the sea ice to measure its thickness. The camera points vertically downwards and takes photos of the are... (Photo: Alfred Wegener Institute / IceCam/Stefan Hendricks)
Luftbild von neugebildetem Meereis Ende September 2012
Aerial image of newly formed sea ice in the end of September 2012
Aerial image of newly formed sea ice in the end of September 2012 (Photo: Alfred Wegener Institute / Stefan Hendricks)
Schmelztuempel auf arktischem Meereis; 

Melt pond on Arctic sea ice.
Melt pond on Arctic sea ice. (Photo: Alfred Wegener Institute / Stefan Hendricks)
Eisstation von Polarstern im Sonnenaufgang
Ice station of Polarstern during dawn
Ice station of Polarstern in the Arctic during dawn (Photo: Alfred Wegener Institute / Stefan Hendricks)
Monatsmittelwerte der Meereisausdehnung im September in der Arktis seit 1979. In Rot der vorraussichtliche Wert für September 2019 +/- zweifache Standardabweichung
Monthly mean of September sea ice extent from 1979 to 2019. The estimated value (+/- two standard deviations) is given in red. (Graphic: Alfred Wegener Institute / meereisportal.de)
Daily Arctic sea ice extent
Daily Arctic sea ice extent including 11September for 2019 (red line). For comparison: the extent for the years 2018, 2017, 2016, 2012, 2007 and the long-term mean from 1981 to 2010 (grey line) and the area of two standard deviations from it (light grey). (Graphic: Alfred Wegener Institute / meereisportal.de)
Karte der Meereisausdehnung am 11. September 2019. Zum Vergleich sind in minimalen Eisausdehnungen 2007 (Rot) und 2012 (Gelb) gezeigt. In beiden Jahren wurden wir die bisher niedrigsten Meereisausdehnungen erreicht. Ergänzend ist die mögliche MOSAiC Startregion in schwarz gekennzeichnet.
Map of the Arctic sea ice extent on 11 September 2019. For comparison, the minimum extent in 2007 (red line) and 2012 (yellow line) are displayed, the years with the lowest summer minima to date. Additionally, the starting region for the MOSAiC expedition with RV Polars... (Graphic: Alfred Wegener Institute / meereisportal.de)