Methane excess in Arctic surface water-triggered by sea ice formation and melting

Arctic amplificaton of global warming has led to increased summer sea ice retreat, which influencesgas exchange between the Arctic Ocean and the atmosphere where sea ice previously acted as a physical barrier. Indeed, recently observed enhanced atmospheric methane concentrations in Arctic regions wi...

Full description

Bibliographic Details
Published in:Scientific Reports
Main Authors: Damm, Ellen, Rudels, Bert, Schauer, Ursula, Mau, Susan, Dieckmann, Gerhard
Format: Article in Journal/Newspaper
Language:unknown
Published: Nature 2015
Subjects:
Online Access:https://epic.awi.de/id/eprint/39023/
https://epic.awi.de/id/eprint/39023/1/srep16179.pdf
https://hdl.handle.net/10013/epic.46252
https://hdl.handle.net/10013/epic.46252.d001
Description
Summary:Arctic amplificaton of global warming has led to increased summer sea ice retreat, which influencesgas exchange between the Arctic Ocean and the atmosphere where sea ice previously acted as a physical barrier. Indeed, recently observed enhanced atmospheric methane concentrations in Arctic regions with fractional sea-ice cover point to unexpected feedbacks in cycling of methane. We report on methane excess in sea ice-influencedwater masses in the interior Arctic Ocean and provide evidence that sea ice is a potential source. We show that methane release from sea ice into the ocean occurs via brine drainage during freezing and melting i.e. in winter and spring. In summer under a fractional sea ice cover, reduced turbulence restricts gas transfer, then seawater acts as bufferin which methane remains entrained. However, in autumn and winter surface convection initiates pronounced effluof methane from the ice covered ocean to the atmosphere. Our results demonstrate that sea ice-sourced methane cycles seasonally between sea ice, sea-ice-influencedseawater and the atmosphere, while the deeper ocean remains decoupled. Freshening due to summer sea ice retreat will enhance this decoupling, which restricts the capacity of the deeper Arctic Ocean to act as a sink for this greenhouse gas.