Atlantic meridional overturning circulation increases flood risk along the United States southeast coast

Abstract The system of oceanic flows constituting the Atlantic Meridional Overturning Circulation (AMOC) moves heat and other properties to the subpolar North Atlantic, controlling regional climate, weather, sea levels, and ecosystems. Climate models suggest a potential AMOC slowdown towards the end...

Full description

Bibliographic Details
Published in:Nature Communications
Main Authors: Denis L. Volkov, Kate Zhang, William E. Johns, Joshua K. Willis, Will Hobbs, Marlos Goes, Hong Zhang, Dimitris Menemenlis
Format: Article in Journal/Newspaper
Language:English
Published: Nature Portfolio 2023
Subjects:
Science
Q
North Atlantic
Online Access:https://doi.org/10.1038/s41467-023-40848-z
https://doaj.org/article/af2e3575ca194e24aad64c87e2c78e4a
Description
Summary:Abstract The system of oceanic flows constituting the Atlantic Meridional Overturning Circulation (AMOC) moves heat and other properties to the subpolar North Atlantic, controlling regional climate, weather, sea levels, and ecosystems. Climate models suggest a potential AMOC slowdown towards the end of this century due to anthropogenic forcing, accelerating coastal sea level rise along the western boundary and dramatically increasing flood risk. While direct observations of the AMOC are still too short to infer long-term trends, we show here that the AMOC-induced changes in gyre-scale heat content, superimposed on the global mean sea level rise, are already influencing the frequency of floods along the United States southeastern seaboard. We find that ocean heat convergence, being the primary driver for interannual sea level changes in the subtropical North Atlantic, has led to an exceptional gyre-scale warming and associated dynamic sea level rise since 2010, accounting for 30-50% of flood days in 2015-2020.

Similar Items