Articles | Volume 22, issue 3
https://doi.org/10.5194/os-22-1763-2026
https://doi.org/10.5194/os-22-1763-2026
Research article
 | 
03 Jun 2026
Research article |  | 03 Jun 2026

On the fate of the Irminger Current water and its impact on the convection region in the Irminger Sea – a Lagrangian model study

Nora Fried, Renske Gelderloos, Oliver J. Tooth, Caroline A. Katsman, and M. Femke de Jong

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Cited articles

Almansi, M. and Gelderloos, R.: OceanSpy: A Python package to facilitate ocean model data analysis and visualization, J. Open Source Softw., 4, https://doi.org/10.21105/joss.01491, 2019. 
Almansi, M., Haine, T. W. N., Pickart, R. S., Magaldi, M. G., Gelderloos, R., and Mastropole, D.: High-Frequency Variability in the Circulation and Hydrography of the Denmark Strait Overflow from a High-Resolution Numerical Model, J. Phys. Oceanogr., 47, 2999–3013, https://doi.org/10.1175/JPO-D-17-0129.1, 2017. 
Almansi, M., Haine, T. W. N., Gelderloos, R., and Pickart, R. S.: Evolution of Denmark Strait Overflow Cyclones and Their Relationship to Overflow Surges, Geophys. Res. Lett., 47, e2019GL086759, https://doi.org/10.1029/2019GL086759, 2020. 
Böning, C. W., Behrens, E., Biastoch, A., Getzlaff, K., and Bamber, J. L.: Emerging impact of Greenland meltwater on deepwater formation in the North Atlantic Ocean, Nat. Geosci., 9, 523–527, https://doi.org/10.1038/ngeo2740, 2016. 
Bromwich, D. H., Wilson, A. B., Bai, L., Liu, Z., Barlage, M., Shih, C.-F., Maldonado, S., Hines, K. M., Wang, S.-H., Woollen, J., Kuo, B., Lin, H.-C., Wee, T.-K., Serreze, M. C., and Walsh, J. E.: The Arctic System Reanalysis, Version 2, B. Am. Meteorol. Soc., 99, 805–828, https://doi.org/10.1175/BAMS-D-16-0215.1, 2018. 
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This study investigates how much warm and saline subtropical-origin water flowing in the Irminger Current (IC) can enter the Irminger Sea convection region by releasing virtual particles in an ocean model. We show that one quarter of IC waters enter the convection region with the potential to increase local stratification. Our results suggest that changes in the water mass properties of the IC have the potential to influence the strength of deep convection in the Irminger Sea.

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