Monitoring One Of The Tipping Points Of The Amoc
Abstract The deep limb of the AMOC is fed by two main sources: a western source generated by deep convection in the Labrador/Irminger seas, and an eastern source originating in overflow of dense water from the Nordic Seas across the Greenland-Scotland Ridge, which is enhanced by water entrained afte...
Main Authors: | , , |
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Format: | Still Image |
Language: | English |
Published: |
Zenodo
2018
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Subjects: | |
Online Access: | https://dx.doi.org/10.5281/zenodo.1188871 https://zenodo.org/record/1188871 |