Hydrofracture: Difference between revisions
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==Ice Shelves== | ==Ice Shelves== | ||
Based on a 2020 assessment, in Antarctica between 50 to 70 percent of ice shelfs that buttress the ice sheet are prone to hydrofracturing. When by atmospheric warming surface meltwater on ice sheets, which is heavier than ice, flows into and enlarges fractures | Based on a 2020 assessment, in Antarctica between 50 to 70 percent of ice shelfs that buttress the ice sheet are prone to hydrofracturing. When by atmospheric warming surface meltwater on ice sheets, which is heavier than ice, flows into and enlarges fractures it can potentially trigger ice-shelf collapse, and in turn threatens to accelerate the retreat of the [[Antarctic Ice Sheet]] - the ice flow and contribution to [[sea-level rise]].<ref>Lai, CY., Kingslake, J., Wearing, M.G. et al. (2020) [https://www.nature.com/articles/s41586-020-2627-8 Vulnerability of Antarctica’s ice shelves to meltwater-driven fracture] Nature</ref> | ||
==See also== | ==See also== | ||
Revision as of 10:39, 7 May 2023
Hydrofracture describes a result by the pressure of freezing water.
Ice Shelves
Based on a 2020 assessment, in Antarctica between 50 to 70 percent of ice shelfs that buttress the ice sheet are prone to hydrofracturing. When by atmospheric warming surface meltwater on ice sheets, which is heavier than ice, flows into and enlarges fractures it can potentially trigger ice-shelf collapse, and in turn threatens to accelerate the retreat of the Antarctic Ice Sheet - the ice flow and contribution to sea-level rise.[1]
See also
References
- ↑ Lai, CY., Kingslake, J., Wearing, M.G. et al. (2020) Vulnerability of Antarctica’s ice shelves to meltwater-driven fracture Nature
