Future shoaling of the AMOC and its impact on oceanic heat transport to the subpolar North Atlantic
The Atlantic Meridional Overturning Circulation (AMOC) carries oceanic heat northward to the subpolar North Atlantic (SPNA), where the surface water cools and sinks to the deep ocean. According to a large-ensemble simulation under a medium-to-high emi
Authors
- Hosmay Lopez (ORCID: https://orcid.org/0000-0002-8422-8699)
- Fabian A. Gomez (ORCID: https://orcid.org/0000-0002-2335-478X)
- Sang‐Ki Lee (ORCID: https://orcid.org/0000-0002-4047-3545)
- Dongmin Kim (ORCID: https://orcid.org/0000-0002-2797-4169)
Institutions
- University of Miami (US)
- NOAA Atlantic Oceanographic and Meteorological Laboratories (US)
- Mississippi State University (US)
Publication Details
- Published
- 2025-09-25
- DOI
- https://doi.org/10.22541/essoar.175883350.02498548/v1
- Primary Topic
- Atmospheric and Environmental Gas Dynamics
- Type
- article
- Field-Weighted Citation Impact
- 0.00
Funders
- University of Miami
- Northern Gulf Institute
- National Oceanic and Atmospheric Administration
- NOAA's Atlantic Oceanographic and Meteorological Laboratory