Articles | Volume 22, issue 3
https://doi.org/10.5194/os-22-1987-2026
https://doi.org/10.5194/os-22-1987-2026
Research article
 | 
26 Jun 2026
Research article |  | 26 Jun 2026

Dynamically downscaled future projections of the Northwest Atlantic Ocean across low to high emissions scenarios

Dongmin Kim, Andrew C. Ross, Sang-Ik Shin, Fabian A. Gomez, Jasmin G. John, Denis L. Volkov, Sang-Ki Lee, Michael A. Alexander, and Charles A. Stock

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Cited articles

Adcroft, A. and Campin, J.-M.: Rescaled height coordinates for accurate representation of free-surface flows in ocean circulation models, Ocean Model., 7, 269–284, https://doi.org/10.1016/j.ocemod.2003.09.003, 2004. 
Adcroft, A. and Hallberg, R.: On methods for solving the oceanic equations of motion in generalized vertical coordinates, Ocean Model., 11, 224–233, https://doi.org/10.1016/j.ocemod.2004.12.007, 2006. 
Alexander, M. A. and Scott, J. D.: The Role of Ekman Ocean Heat Transport in the Northern Hemisphere Response to ENSO, J. Climate, 21, 5688–5707, https://doi.org/10.1175/2008JCLI2382.1, 2008. 
Alexander, M. A., Shin, S., Scott, J. D., Curchitser, E., and Stock, C.: The Response of the Northwest Atlantic Ocean to Climate Change, J. Climate, 33, 405–428, https://doi.org/10.1175/JCLI-D-19-0117.1, 2020. 
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Short summary
Using high-resolution Modular Ocean Model version 6, we projected Northwest Atlantic changes under four future emission scenarios. Results show a weakening Gulf Stream reduces upwelling, causing significant shelf warming and salinification. This also leads to dynamic sea-level rise along the US East Coast, particularly in the South Atlantic Bight, with critical implications for marine ecosystems and coastal risks.
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