Email this article Stability of continental relic methane hydrates for the holocene climatic optimum and for contemporary conditions
- Authors: Arzhanov M.M.1, Mokhov I.I.1,2
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Affiliations:
- Obukhov Institute of Atmospheric Physics
- Faculty of Physics
- Issue: Vol 476, No 2 (2017)
- Pages: 1163-1167
- Section: Geophysics
- URL: https://ogarev-online.ru/1028-334X/article/view/191049
- DOI: https://doi.org/10.1134/S1028334X17100026
- ID: 191049
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Abstract
Modelling of the thermal regime of permafrost soils has made it possible to estimate the stability of methane hydrates in the continental permafrost in the Northern Eurasian and North American regions with the risk of gas emissions into the atmosphere as a result of possible dissociation of gas hydrates in the Holocene Optimum and under contemporary climatic conditions [1, 2].
About the authors
M. M. Arzhanov
Obukhov Institute of Atmospheric Physics
Author for correspondence.
Email: arzhanov@ifaran.ru
Russian Federation, Moscow, 119017
I. I. Mokhov
Obukhov Institute of Atmospheric Physics; Faculty of Physics
Email: arzhanov@ifaran.ru
Russian Federation, Moscow, 119017; Moscow, 119991
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