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 |
---|---|
Main Authors: | , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Copernicus Publications
2018
|
Subjects: | |
Online Access: | https://doi.org/10.5194/tc-12-2955-2018 https://noa.gwlb.de/receive/cop_mods_00004626 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00004583/tc-12-2955-2018.pdf https://tc.copernicus.org/articles/12/2955/2018/tc-12-2955-2018.pdf |