Stopping the flood: could we use targeted geoengineering to mitigate sea level rise?
The Marine Ice Sheet Instability (MISI) is a dynamic feedback that can cause an ice sheet to enter a runaway collapse. Thwaites Glacier, West Antarctica, is projected to be the largest individual source of future sea level rise and may have already entered MISI. Here, we use a suite of coupled quasi...
Published in: | The Cryosphere |
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Main Authors: | , |
Format: | Text |
Language: | English |
Published: |
2018
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Subjects: | |
Online Access: | https://doi.org/10.5194/tc-12-2955-2018 https://tc.copernicus.org/articles/12/2955/2018/ |