A. Trivedi
Reassessment of hydrate destabilization mechanisms offshore west Svalbard confirms link to recent ocean warming
Trivedi, A.; Sarkar, S.; Marin-Moreno, H.; Minshull, T.A.; Whitehouse, P.L.; Singh, U.
Authors
S. Sarkar
H. Marin-Moreno
T.A. Minshull
Professor Pippa Whitehouse pippa.whitehouse@durham.ac.uk
Honorary Professor
U. Singh
Abstract
The stability of methane hydrates at the feather edge of hydrate stability on the upper continental slope (UCS) is prone to ocean warming and relative sea-level (RSL) change. West of Svalbard, methane seeps on the UCS were initially proposed to result from hydrate destabilization resulting from four decades of warming of Atlantic bottom water. Alternatively, it has been proposed that hydrate dissociation was triggered by RSL fall due to isostatic rebound over the past 8000 years rather than recent bottom water temperature (BWT) rise. Here we address these two contrasting hypotheses by simulating the impact of 11000 years of BWT and RSL change on hydrates located at the UCS off west Svalbard. Our numerical simulation considers multiphase fluid and heat flow coupled with hydrate formation and dissociation. We used two reconstructions of local ice history (UiT and ICE-6G_C) that predict contrasting results for the local sea-level history. Over the past 8000 years, the UiT model predicts a fall in RSL on the UCS, while the ICE-6G_C model, which provides a better fit to nearby coastal RSL observations, predicts a continuous rise. Our modeling shows that whilst long-term RSL fall would progressively thin the region of hydrate stability, the abrupt rise in BWT enhances hydrate dissociation. Even in the model with an RSL rise, the increase in BWT causes hydrate destabilization and pore water freshening that matches observations. We conclude that recent ocean warming plays a critical role in hydrate dissociation west of Svalbard regardless of the longer term sea-level history.
Citation
Trivedi, A., Sarkar, S., Marin-Moreno, H., Minshull, T., Whitehouse, P., & Singh, U. (2022). Reassessment of hydrate destabilization mechanisms offshore west Svalbard confirms link to recent ocean warming. Journal of Geophysical Research. Solid Earth, 127(11), Article e2022JB025231. https://doi.org/10.1029/2022jb025231
Journal Article Type | Article |
---|---|
Acceptance Date | Oct 14, 2022 |
Online Publication Date | Oct 20, 2022 |
Publication Date | 2022-11 |
Deposit Date | Oct 21, 2022 |
Publicly Available Date | Oct 24, 2022 |
Journal | Journal of Geophysical Research - Solid Earth |
Print ISSN | 2169-9313 |
Electronic ISSN | 2169-9356 |
Publisher | American Geophysical Union |
Peer Reviewed | Peer Reviewed |
Volume | 127 |
Issue | 11 |
Article Number | e2022JB025231 |
DOI | https://doi.org/10.1029/2022jb025231 |
Public URL | https://durham-repository.worktribe.com/output/1191138 |
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Copyright Statement
An edited version of this paper was published by AGU. Copyright (2022) American Geophysical Union
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