Abstract
Vast quantities of gas hydrate could be trapped in the Arctic Ocean, and there is concern that a rise in the ocean temperatures could induce dissociation of these hydrate accumulations, potentially releasing large amounts of methane. In first approximation, the hydrate is not stable in the Arctic shelf because of the low pressure (shallow water), but if we consider presence of sub-sea permafrost in this area the hydrate can be stable. In this context, we define the areas where conditions prevail for gas hydrates stability in the Arctic shelf versus sub-sea permafrost thickness, temperature and geothermal gradient.
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Acknowledgments
The authors wish to thank Manuela Sedmach for the graphic support. The authors largely benefited from suggestions of two anonymous journal reviewers.
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This peer-reviewed article is a result of the multi and interdisciplinary research activities based at the Arctic Station “Dirigibile Italia”, coordinated by the “Dipartimento Scienze del Sistema Terra e Tecnologie per l’Ambiente” of the National Research Council of Italy.
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Tinivella, U., Giustiniani, M. Gas hydrate stability zone in shallow Arctic Ocean in presence of sub-sea permafrost. Rend. Fis. Acc. Lincei 27 (Suppl 1), 163–171 (2016). https://doi.org/10.1007/s12210-016-0520-z
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DOI: https://doi.org/10.1007/s12210-016-0520-z