The Arctic Ocean in summer will very likely be ice-free before 2050, at least temporally. The efficacy of climate-protection measures will determine how often and for how long. These are the results of a new research study involving 21 research institutes from around the world, coordinated by Dirk Notz from the University of Hamburg, Germany.
The research team has analyzed recent results from 40 different climate models. Using these models, the researchers considered the future evolution of Arctic sea-ice cover in a scenario with high future CO2 emissions and little climate protection. As expected, Arctic sea ice disappeared quickly in summer in these simulations. However, the new study finds that Arctic summer sea ice also disappears occasionally if CO2 emissions are rapidly reduced.
“If we reduce global emissions rapidly and substantially, and thus keep global warming below 2 °C relative to preindustrial levels, Arctic sea ice will nevertheless likely disappear occasionally in summer even before 2050. This really surprised us” said Dirk Notz, who leads the sea-ice research group at University of Hamburg, Germany.
Currently, the North Pole is covered by sea ice year-round. Each summer, the area of the sea ice cover decreases, and in winter it grows again. In response to ongoing global warming, the overall area of the Arctic Ocean that is covered by sea ice has rapidly been reduced over the past few decades. This substantially affects the Arctic ecosystem and climate: The sea-ice cover is a hunting ground and habitat for polar bears and seals, and keeps the Arctic cool by reflecting sunlight.
How often the Arctic will lose its sea-ice cover in the future critically depends on future CO2 emissions, the study shows. If emissions are reduced rapidly, ice-free years only occur occasionally. With higher emissions, the Arctic Ocean will become ice free in most years. Hence, humans still have an impact on how often the Arctic loses its year-round sea-ice cover.
Reference: “Arctic Sea Ice in CMIP6” by Dirk Notz, Jakob Dörr, David A. Bailey, Ed Blockley, Mitchell Bushuk, Jens Boldingh Debernard, Evelien Dekker, Patricia DeRepentigny, David Docquier, Neven S. Fuckar, John C. Fyfe, Alexandra Jahn, Marika Holland, Elizabeth Hunke, Doroteaciro Iovino, Narges Khosravi, Francois Massonnet, Gurvan Madec, Siobhan O’Farrell, Alek Petty, Arun Rana, Lettie Roach, Erica Rosenblum, Clement Rousset, Tido Semmler, Julienne Stroeve, Bruno Tremblay, Takahiro Toyoda, Hiroyuki Tsujino and Martin Vancoppenolle, 17 April 2020, Geophysical Research Letters.
DOI: 10.1029/2019GL086749
Technical Details: The simulations used in this study are based on so-called SSP Scenarios (shared socio-economic pathways), which will also be used for the next IPCC report. Scenarios SSP1-1.9 and SSP1-2.6 are used to simulate a rapid reduction of future CO2 emissions, while scenario SSP5-8.5 is used to simulate largely unchanged future CO2 emissions. The study is based on simulations from the most recent generation of climate models, collected within the Coupled Model Intercomparison Project Phase 6 (CMIP6).
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