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7 November 2019

 

Erosion of permafrost coasts in the Arctic could vent major amounts of CO2

Permafrost coasts make up about one third of the Earth’s total coastline. As a result of accelerated climate change, whole sections of coastline rapidly thaw and erode into the Arctic Ocean. A study published in the journal Geophysical Research Letters now shows that large amounts of carbon dioxide are potentially being produced along these eroding permafrost coastlines in the Arctic.


“Carbon budgets and climate simulations have so far missed coastal erosion in their equations even though it might be a substantial source of carbon dioxide,” says George Tanski of Vrije Universiteit Amsterdam, lead author of the study. “Our research found that the erosion of permafrost coastlines can lead to the rapid release of significant quantities of CO2, which can be expected to increase as coastal erosion accelerates, temperatures increase, sea ice diminishes, and stronger storms batter Arctic coasts.”


Simulating erosion effects in the lab

For the study, the researchers simulated the effects of erosion in a lab experiment. To find out how much carbon is released into the atmosphere along eroding Arctic permafrost coasts, they collected permafrost samples from Qikiqtaruk (also known as Herschel Island) off the northern coast of the Yukon in northwest Canada, and seawater from offshore. They mixed permafrost and seawater samples and then measured the greenhouse gases emitted over the course of four months, the average length of open-water season in the Arctic.


The researchers found that CO2 was released as rapidly from thawing permafrost in seawater as it is from thawing permafrost on land. Previous research had documented that thawing permafrost on land causes significant releases of greenhouse gases. This new research indicates that eroding permafrost coasts and nearshore waters are also a potentially notable source of CO2 emissions. It draws into question carbon budgets that have identified the coastal zone mainly as a point of passage for carbon from land to sea, neglecting possible carbon transport into the atmosphere.


The study was carried out during Tanski’s time at the Alfred Wegener Institute (AWI), Helmholtz Centre for Polar and Marine Research, and the GFZ German Research Centre for Geosciences. Co-authors come from AWI, GFZ, the University of Hamburg, and the University of Potsdam. The study is part of the Nunataryuk research project, which aims to assess permafrost thaw, study how it contributes to climate change, understand its impacts on indigenous communities and other people, and develop mitigation and adaptation strategies. The project brings together world-leading specialists in natural science and socio-economics and connects them with stakeholders from around the Arctic coast. Nunataryuk is an EU-funded Horizon 2020 project coordinated by the Alfred Wegener Institute in Potsdam, Germany.


Original study:

Tanski, G., Wagner, D., Knoblauch, C., Fritz, M., Sachs, T., Lantuit, H., 2019. Rapid CO2 Release From Eroding Permafrost in Seawater. Geophysical Research Letters. DOI: 10.1029/2019GL084303

 
Scientific contact:

Dr. George Tanski
Vrije Universiteit Amsterdam
Telephone: +31 644 804 694
Email: This email address is being protected from spambots. You need JavaScript enabled to view it.

 

Media relations contact:

Dipl.-Phys. Philipp Hummel
Public and Media Relations
Helmholtz Centre Potsdam GFZ
German Research Centre for Geosciences
Telegrafenberg
14473 Potsdam
Telephone: +49 331 288-1049
Email: This email address is being protected from spambots. You need JavaScript enabled to view it.

 

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