Articles | Volume 16, issue 2
https://doi.org/10.5194/os-16-451-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/os-16-451-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Barotropic vorticity balance of the North Atlantic subpolar gyre in an eddy-resolving model
Mathieu Le Corre
CORRESPONDING AUTHOR
Laboratoire d'Océanographie Physique et Spatiale (LOPS), Univ. Brest, CNRS, IRD, Ifremer, IUEM, Brest, France
Jonathan Gula
Laboratoire d'Océanographie Physique et Spatiale (LOPS), Univ. Brest, CNRS, IRD, Ifremer, IUEM, Brest, France
Anne-Marie Tréguier
Laboratoire d'Océanographie Physique et Spatiale (LOPS), Univ. Brest, CNRS, IRD, Ifremer, IUEM, Brest, France
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- Oceanic Mesoscale Eddy Depletion Catalyzed by Internal Waves R. Barkan et al. 10.1029/2021GL094376
- Decadal variability of eddy temperature fluxes in the Labrador Sea C. Danek et al. 10.1016/j.ocemod.2023.102170
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- A Southern Ocean supergyre as a unifying dynamical framework identified by physics-informed machine learning M. Sonnewald et al. 10.1038/s43247-023-00793-7
- On the risk of abrupt changes in the North Atlantic subpolar gyre in CMIP6 models D. Swingedouw et al. 10.1111/nyas.14659
- Cloud-based framework for inter-comparing submesoscale-permitting realistic ocean models T. Uchida et al. 10.5194/gmd-15-5829-2022
- Freshwater routing in eddy-permitting simulations of the last deglacial: the impact of realistic freshwater discharge R. Love et al. 10.5194/cp-17-2327-2021
- Ocean Barotropic Vorticity Balances: Theory and Application to Numerical Models R. Waldman & H. Giordani 10.1029/2022MS003276
- Circulation adjustment in the Arctic and Atlantic in response to Greenland and Antarctic mass loss J. Berk et al. 10.1007/s00382-021-05755-3
- Flow‐Topography Interaction Along the Spanish Slope in the Alboran Sea: Vorticity Generation and Connection to Interior Fronts E. Capó et al. 10.1029/2022JC019480
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- The influence of merger and convection on an anticyclonic eddy trapped in a bowl C. de Marez et al. 10.1016/j.ocemod.2021.101874
- Coaction of Top and Bottom Drags in Gulf Stream Dynamics L. Renault et al. 10.1029/2022JC018939
- Spurious Forces Can Dominate the Vorticity Budget of Ocean Gyres on the C‐Grid A. Styles et al. 10.1029/2021MS002884
- Opportunities for Earth Observation to Inform Risk Management for Ocean Tipping Points R. Wood et al. 10.1007/s10712-024-09859-3
- Energy Spectra and Vorticity Dynamics in a Two-Layer Shallow Water Ocean Model N. Kevlahan & F. Poulin 10.1175/JPO-D-21-0318.1
22 citations as recorded by crossref.
- AMOC Recent and Future Trends: A Crucial Role for Oceanic Resolution and Greenland Melting? D. Swingedouw et al. 10.3389/fclim.2022.838310
- Why Does the Deep Western Boundary Current “Leak” around Flemish Cap? A. Solodoch et al. 10.1175/JPO-D-19-0247.1
- Oceanic Mesoscale Eddy Depletion Catalyzed by Internal Waves R. Barkan et al. 10.1029/2021GL094376
- Decadal variability of eddy temperature fluxes in the Labrador Sea C. Danek et al. 10.1016/j.ocemod.2023.102170
- On the Influence of the Current Feedback to the Atmosphere on the Western Mediterranean Sea Dynamics L. Renault et al. 10.1029/2020JC016664
- A Persistent Deep Anticyclonic Vortex in the Rockall Trough Sustained by Anticyclonic Vortices Shed From the Slope Current and Wintertime Convection A. Smilenova et al. 10.1029/2019JC015905
- On the Role of Bottom Pressure Torques in Wind-Driven Gyres A. Stewart et al. 10.1175/JPO-D-20-0147.1
- High-resolution stochastic downscaling method for ocean forecasting models and its application to the Red Sea dynamics G. Shapiro et al. 10.5194/os-17-891-2021
- On the dynamics of the Ross Gyre: the relative importance of wind, buoyancy, eddies, and the Antarctic Circumpolar Current Y. Wang et al. 10.3389/fmars.2024.1465808
- A Southern Ocean supergyre as a unifying dynamical framework identified by physics-informed machine learning M. Sonnewald et al. 10.1038/s43247-023-00793-7
- On the risk of abrupt changes in the North Atlantic subpolar gyre in CMIP6 models D. Swingedouw et al. 10.1111/nyas.14659
- Cloud-based framework for inter-comparing submesoscale-permitting realistic ocean models T. Uchida et al. 10.5194/gmd-15-5829-2022
- Freshwater routing in eddy-permitting simulations of the last deglacial: the impact of realistic freshwater discharge R. Love et al. 10.5194/cp-17-2327-2021
- Ocean Barotropic Vorticity Balances: Theory and Application to Numerical Models R. Waldman & H. Giordani 10.1029/2022MS003276
- Circulation adjustment in the Arctic and Atlantic in response to Greenland and Antarctic mass loss J. Berk et al. 10.1007/s00382-021-05755-3
- Flow‐Topography Interaction Along the Spanish Slope in the Alboran Sea: Vorticity Generation and Connection to Interior Fronts E. Capó et al. 10.1029/2022JC019480
- Predicting particle catchment areas of deep-ocean sediment traps using machine learning T. Picard et al. 10.5194/os-20-1149-2024
- The influence of merger and convection on an anticyclonic eddy trapped in a bowl C. de Marez et al. 10.1016/j.ocemod.2021.101874
- Coaction of Top and Bottom Drags in Gulf Stream Dynamics L. Renault et al. 10.1029/2022JC018939
- Spurious Forces Can Dominate the Vorticity Budget of Ocean Gyres on the C‐Grid A. Styles et al. 10.1029/2021MS002884
- Opportunities for Earth Observation to Inform Risk Management for Ocean Tipping Points R. Wood et al. 10.1007/s10712-024-09859-3
- Energy Spectra and Vorticity Dynamics in a Two-Layer Shallow Water Ocean Model N. Kevlahan & F. Poulin 10.1175/JPO-D-21-0318.1
Latest update: 10 Dec 2024
Short summary
The ocean circulation is crucial for the climate, and the North Atlantic subpolar gyre is a key component of the meridional heat transport. In this study we use a high-resolution simulation with bottom-following coordinates to investigate the gyre dynamics. We show that nonlinear processes, underestimated in most climate models, control the circulation in the gyre interior. This result contrasts with the classical theory putting forward wind effects on the large-scale circulation.
The ocean circulation is crucial for the climate, and the North Atlantic subpolar gyre is a key...