Sea-ice-free Arctic makes permafrost vulnerable to thawing

Sea-ice-free Arctic makes permafrost vulnerable to thawing
Researchers gathering data in a Siberian cave. Credit: University of Oxford

Permafrost is ground that remains frozen throughout the year; it covers nearly a quarter of Northern Hemisphere land. The frozen state of permafrost enables it to store large amounts of carbon; about twice as much as in the atmosphere. The rate and extent of future thawing of permafrost, and consequent release of its carbon, is hard to predict from modern observations alone.

However, a crucial past relationship between summer sea ice in the Arctic and , discovered in this study, is now understood, with significant implications for the future.

Prof. Gideon Henderson, an author of the study based at the Department of Earth Sciences, University of Oxford, said: 'We were surprised to find that times when permafrost melted in the past did not simply match up with times when the Earth was at its warmest, but were much more likely when the Arctic was free of ice in the summer. This discovery about the past behaviour of permafrost suggests that the expected loss of Arctic sea ice in the future will accelerate melting of the permafrost presently found across much of Siberia.'

Significant decreases of Arctic sea ice have been observed in recent years, and the Arctic is expected to be free of summer sea ice in the coming decades. Such loss of sea ice is likely to lead to an acceleration of thawing of permafrost in Siberia and to consequent release of carbon.

The new research relies on challenging to discover and explore Siberian caves. Caves are powerful recorders of periods when permafrost was absent in the past. Stalagmites, stalactites and flowstones can only form when there is liquid water, and therefore not when overlying land is permanently frozen. The presence of stalagmites in caves under present permafrost thus demonstrate periods when permafrost was absent in the past.

Development of new approaches to date stalagmites using measurements of natural uranium and lead, allow dating of the recovered stalagmites—and therefore of periods of permafrost absence—for the last one and a half million years. Stalagmites grew intermittently from 1,500,000 to 400,000 years ago, and have not grown for the last 400,000 years. The timing of formation, and therefore absence of permafrost, do not relate simply to global temperatures in the past but are notably more common when the Arctic Ocean was free of summer sea-ice.

This study shows that several processes may lead to the relationship between Arctic sea-ice and permafrost. The absence of sea ice leads to an increase in heat and moisture transfer from ocean to atmosphere and therefore to warmer air transported far overland into Siberia. Moisture transport also increases snow fall over Siberia during the autumn months. This blanket of snow insulates the ground from the extreme cold of winters leading to an increase in average annual ground temperatures, destabilising the permafrost. Consequently, in regions with increased and insulation, permafrost will start to thaw, releasing carbon dioxide that was trapped for millennia.

The paper—'Palaeoclimate evidence of vulnerable permafrost during times of low sea ice'—will be available online at Nature on 8 January 2020,


Explore further

Western Siberian rivers and lakes emit greenhouse gases into the atmosphere

More information: Palaeoclimate evidence of vulnerable permafrost during times of low sea ice, Nature, DOI: 10.1038/s41586-019-1880-1 , https://nature.com/articles/s41586-019-1880-1
Journal information: Nature

Citation: Sea-ice-free Arctic makes permafrost vulnerable to thawing (2020, January 8) retrieved 21 February 2020 from https://phys.org/news/2020-01-sea-ice-free-arctic-permafrost-vulnerable.html
This document is subject to copyright. Apart from any fair dealing for the purpose of private study or research, no part may be reproduced without the written permission. The content is provided for information purposes only.
350 shares

Feedback to editors

User comments