17 citations as recorded by crossref.

1. Oxygen export to the deep ocean following Labrador Sea Water formation J. Koelling et al. https://doi.org/10.5194/bg-19-437-2022
2. Subpolar North Atlantic western boundary density anomalies and the Meridional Overturning Circulation F. Li et al. https://doi.org/10.1038/s41467-021-23350-2
3. Wind‐Forced Upwelling Along the West Greenland Shelfbreak: Implications for Labrador Sea Water Formation A. Pacini & R. Pickart https://doi.org/10.1029/2022JC018952
4. New insights into the eastern subpolar North Atlantic meridional overturning circulation from OVIDE H. Mercier et al. https://doi.org/10.5194/os-20-779-2024
5. Preparing the New Phase of Argo: Scientific Achievements of the NAOS Project P. Le Traon et al. https://doi.org/10.3389/fmars.2020.577408
6. Meanders of the West Greenland Current near Cape Farewell A. Pacini & R. Pickart https://doi.org/10.1016/j.dsr.2021.103664
7. Labrador sea water spreading and the Atlantic meridional overturning circulation I. Le Bras https://doi.org/10.1098/rsta.2022.0189
8. Coherence of Deep Convection in the Irminger Sea with Oceanic Heat Advection D. Iakovleva et al. https://doi.org/10.1134/S0001437023070214
9. On the ocean's response to enhanced Greenland runoff in model experiments: relevance of mesoscale dynamics and atmospheric coupling T. Martin & A. Biastoch https://doi.org/10.5194/os-19-141-2023
10. Delayed Recovery of the Irminger Interior From Cooling in 2015 Due To Widespread Buoyancy Loss and Suppressed Restratification M. Nelson et al. https://doi.org/10.1029/2023GL106501
11. Changing Spatial Patterns of Deep Convection in the Subpolar North Atlantic S. Rühs et al. https://doi.org/10.1029/2021JC017245
12. Deep convection in the Subpolar Gyre: Do we have enough data to estimate its intensity? A. Fedorov et al. https://doi.org/10.1016/j.dynatmoce.2022.101338
13. Ekman Transport as the Driver of Extreme Interannual Formation Rates of Eighteen Degree Water K. Li et al. https://doi.org/10.1029/2021JC017696
14. The redistribution of anthropogenic excess heat is a key driver of warming in the North Atlantic M. Messias & H. Mercier https://doi.org/10.1038/s43247-022-00443-4
15. Seasonal to long-term variability of natural and anthropogenic carbon concentrations and transports in the subpolar North Atlantic Ocean R. Bajon et al. https://doi.org/10.5194/bg-23-2335-2026
16. On the fate of the Irminger Current water and its impact on the convection region in the Irminger Sea – a Lagrangian model study N. Fried et al. https://doi.org/10.5194/os-22-1763-2026
17. Arrival of New Great Salinity Anomaly Weakens Convection in the Irminger Sea T. Biló et al. https://doi.org/10.1029/2022GL098857