Articles | Volume 13, issue 10
https://doi.org/10.5194/gmd-13-4959-2020
© 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/gmd-13-4959-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Model experiment description paper
| 
19 Oct 2020
Model experiment description paper |
| 19 Oct 2020
| 19 Oct 2020
Introducing LAB60: A 1∕60° NEMO 3.6 numerical simulation of the Labrador Sea
Clark Pennelly
CORRESPONDING AUTHOR
Earth Sciences Building, University of Alberta, Edmonton, Alberta, T6G 2E3, Canada
Paul G. Myers
Earth Sciences Building, University of Alberta, Edmonton, Alberta, T6G 2E3, Canada
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Cited
16 citations as recorded by crossref.
- Evaluation of the CMCC global eddying ocean model for the Ocean Model Intercomparison Project (OMIP2) D. Iovino et al. 10.5194/gmd-16-6127-2023
- The Impacts of Air-Sea Fluxes and Model Resolution on Seasonal and Inter-Annual Variability of the Atlantic Meridional Overturning Circulation across the OSNAP West Section P. Hoshyar et al. 10.1016/j.ocemod.2023.102307
- Mechanisms of Heat Flux Across the Southern Greenland Continental Shelf in 1/10° and 1/12° Ocean/Sea Ice Simulations T. Morrison et al. 10.1029/2022JC019021
- Ocean Modeling with Adaptive REsolution (OMARE; version 1.0) – refactoring the NEMO model (version 4.0.1) with the parallel computing framework of JASMIN – Part 1: Adaptive grid refinement in an idealized double-gyre case Y. Zhang et al. 10.5194/gmd-16-679-2023
- Seasonal overturning variability in the eastern North Atlantic subpolar gyre: a Lagrangian perspective O. Tooth et al. 10.5194/os-19-769-2023
- Winter Mixed Layer Restratification Induced by Vertical Eddy Buoyancy Flux in the Labrador Sea P. Li et al. 10.1029/2023GL103341
- Wind‐Forced Upwelling Along the West Greenland Shelfbreak: Implications for Labrador Sea Water Formation A. Pacini & R. Pickart 10.1029/2022JC018952
- Impact of Ocean Heat Transport on Arctic Sea Ice Variability in the GFDL CM2‐O Model Suite M. Decuypère et al. 10.1029/2021JC017762
- A regional NEMO 4.0 configuration of the subpolar North Atlantic P. Verezemskaya et al. 10.1016/j.ocemod.2024.102457
- Relative Contribution of Atmospheric Forcing, Oceanic Preconditioning and Sea Ice to Deep Convection in the Labrador Sea Y. Wu et al. 10.3390/jmse11040869
- Shifts from surface density compensation to projected warming, freshening and stronger stratification in the subpolar North Atlantic R. Marsh et al. 10.1007/s00382-024-07336-6
- Tracking Irminger Rings’ properties using a sub-mesoscale ocean model C. Pennelly & P. Myers 10.1016/j.pocean.2021.102735
- Meanders of the West Greenland Current near Cape Farewell A. Pacini & R. Pickart 10.1016/j.dsr.2021.103664
- Changing Spatial Patterns of Deep Convection in the Subpolar North Atlantic S. Rühs et al. 10.1029/2021JC017245
- The Changing Behavior of the West Greenland Current System in a Very High‐Resolution Model R. Gou et al. 10.1029/2022JC018404
- Seasonal Cycle of the Coastal West Greenland Current System Between Cape Farewell and Cape Desolation From a Very High‐Resolution Numerical Model R. Gou et al. 10.1029/2020JC017017
14 citations as recorded by crossref.
- Evaluation of the CMCC global eddying ocean model for the Ocean Model Intercomparison Project (OMIP2) D. Iovino et al. 10.5194/gmd-16-6127-2023
- The Impacts of Air-Sea Fluxes and Model Resolution on Seasonal and Inter-Annual Variability of the Atlantic Meridional Overturning Circulation across the OSNAP West Section P. Hoshyar et al. 10.1016/j.ocemod.2023.102307
- Mechanisms of Heat Flux Across the Southern Greenland Continental Shelf in 1/10° and 1/12° Ocean/Sea Ice Simulations T. Morrison et al. 10.1029/2022JC019021
- Ocean Modeling with Adaptive REsolution (OMARE; version 1.0) – refactoring the NEMO model (version 4.0.1) with the parallel computing framework of JASMIN – Part 1: Adaptive grid refinement in an idealized double-gyre case Y. Zhang et al. 10.5194/gmd-16-679-2023
- Seasonal overturning variability in the eastern North Atlantic subpolar gyre: a Lagrangian perspective O. Tooth et al. 10.5194/os-19-769-2023
- Winter Mixed Layer Restratification Induced by Vertical Eddy Buoyancy Flux in the Labrador Sea P. Li et al. 10.1029/2023GL103341
- Wind‐Forced Upwelling Along the West Greenland Shelfbreak: Implications for Labrador Sea Water Formation A. Pacini & R. Pickart 10.1029/2022JC018952
- Impact of Ocean Heat Transport on Arctic Sea Ice Variability in the GFDL CM2‐O Model Suite M. Decuypère et al. 10.1029/2021JC017762
- A regional NEMO 4.0 configuration of the subpolar North Atlantic P. Verezemskaya et al. 10.1016/j.ocemod.2024.102457
- Relative Contribution of Atmospheric Forcing, Oceanic Preconditioning and Sea Ice to Deep Convection in the Labrador Sea Y. Wu et al. 10.3390/jmse11040869
- Shifts from surface density compensation to projected warming, freshening and stronger stratification in the subpolar North Atlantic R. Marsh et al. 10.1007/s00382-024-07336-6
- Tracking Irminger Rings’ properties using a sub-mesoscale ocean model C. Pennelly & P. Myers 10.1016/j.pocean.2021.102735
- Meanders of the West Greenland Current near Cape Farewell A. Pacini & R. Pickart 10.1016/j.dsr.2021.103664
- Changing Spatial Patterns of Deep Convection in the Subpolar North Atlantic S. Rühs et al. 10.1029/2021JC017245
2 citations as recorded by crossref.
- The Changing Behavior of the West Greenland Current System in a Very High‐Resolution Model R. Gou et al. 10.1029/2022JC018404
- Seasonal Cycle of the Coastal West Greenland Current System Between Cape Farewell and Cape Desolation From a Very High‐Resolution Numerical Model R. Gou et al. 10.1029/2020JC017017
Latest update: 17 Nov 2024
Short summary
A high-resolution ocean simulation was carried out within the Labrador Sea, a region that low-resolution climate simulations may misrepresent. We show that small-scale eddies and their associated transport are better resolved at higher resolution than at lower resolution. These eddies transport important properties to the interior of the Labrador Sea, impacting the stratification and reducing the convection extent so that it is far more accurate when compared to what observations suggest.
A high-resolution ocean simulation was carried out within the Labrador Sea, a region that...
