ATLAS 5th General Assembly - Atlantic Paleo Circulation: A long-term context for the modern Ocean

• Exceptionally weak industrial-era AMOC (caused by weak LSW and ISOW). • Has AMOC weakening continued through the 20th century? Relative cooling of SPG may be related to horizontal gyre circulation rather than deep components of AMOC. • Unprecedented 20th century changes in subpolar gyre circulatio...

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Bibliographic Details
Main Authors: Thornalley, David, Spooner, Peter
Format: Conference Object
Language:unknown
Published: 2020
Subjects:
Online Access:https://zenodo.org/record/3760556
https://doi.org/10.5281/zenodo.3760556
Description
Summary:• Exceptionally weak industrial-era AMOC (caused by weak LSW and ISOW). • Has AMOC weakening continued through the 20th century? Relative cooling of SPG may be related to horizontal gyre circulation rather than deep components of AMOC. • Unprecedented 20th century changes in subpolar gyre circulation caused pronounced changes in Northeast Atlantic hydrography and ecosystems. • Recent variability is not simply ‘typical ongoing decadal variability’. Likely future no-analogue conditions. Reliance on climate model projections. • Better understanding of post Little Ice Age and 20th century changes is required for assessing climate model sensitivity and projections of AMOC.