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: |
2018
|
Subjects: | |
Online Access: | https://research.ulapland.fi/fi/publications/bbb28a0a-86d1-425b-92ec-c601286ac730 https://doi.org/10.5194/tc-12-2955-2018 http://www.scopus.com/inward/record.url?scp=85053905908&partnerID=8YFLogxK http://www.scopus.com/inward/citedby.url?scp=85053905908&partnerID=8YFLogxK |