The effect of model bias on Atlantic freshwater transport and implications for AMOC bi-stability
Evidence from paleo-proxy records suggests that the Atlantic Meridional Overturning Circulation (AMOC) can be in both an AMOC on state, the AMOC as we observe it today, and an AMOC off state, where the AMOC becomes extremely weak or even collapses. The freshwater transport due to the AMOC ($ M_{ov}...
Main Authors: | , , , |
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Format: | Article |
Language: | English |
Published: |
Stockholm University Press
2017-01-01
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Series: | Tellus: Series A, Dynamic Meteorology and Oceanography |
Subjects: | |
Online Access: | http://dx.doi.org/10.1080/16000870.2017.1299910 |