Articles | Volume 19, issue 16
https://doi.org/10.5194/gmd-19-7939-2026
https://doi.org/10.5194/gmd-19-7939-2026
Model description paper
 | 
26 Aug 2026
Model description paper |  | 26 Aug 2026

Turbulence-driven nutrient supply sustains ice-algal growth in the Arctic: a modeling approach with CICE 6.1 coupled to Icepack 1.2, and with SIMBA 2.0

Giulia Castellani, Karley Campbell, Sebastien Moreau, and Pedro Duarte

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Cited articles

Angelopoulos, M., Damm, E., Simões Pereira, P., Abrahamsson, K., Bauch, D., Bowman, J., Castellani, G., Creamean, J., Divine, D. V., Dumitrascu, A., Fons, S. W., Granskog, M. A., Kolabutin, N., Krumpen, T., Marsay, C., Nicolaus, M., Oggier, M., Rinke, A., Sachs, T., Shimanchuk, E., Stefels, J., Stephens, M., Ulfsbo, A., Verdugo, J., Wang, L., Zhan, L., and Haas, C.: Deciphering the Properties of Different Arctic Ice Types During the Growth Phase of MOSAiC: Implications for Future Studies on Gas Pathways, Front. Earth Sci., 10, 2022, https://doi.org/10.3389/feart.2022.864523, 2022. a, b
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Ayata, S.-D., Lévy, M., Aumont, O., Sciandra, A., Sainte-Marie, J., Tagliabue, A., and Bernard, O.: Phytoplankton growth formulation in marine ecosystem models: Should we take into account photo-acclimation and variable stoichiometry in oligotrophic areas?, J. Mar. Syst., 125, 29–40, https://doi.org/10.1016/j.jmarsys.2012.12.010, 2013. a
Boetius, A., Albrecht, S., Bakker, K., Bienhold, C., Felden, J., Fernández-Méndez, M., Hendricks, S., Katlein, C., Lalande, C., Krumpen, T., Nicolaus, M., Peeken, I., Rabe, B., Rogacheva, A., Rybakova, E., Somavilla, R., Wenzhöfer, F., and and RV Polarstern ARK27-3-Shipboard science party: Export of Algal Biomass from the Melting Arctic Sea Ice, Science, 339, 1430–1432, https://doi.org/10.1126/science.1231346, 2013. a
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Nutrient exchange at the ocean-ice interface is a key process to supply nutrients and support sea-ice algal growth in polar regions. Such fluxes depend on the characteristics of the flow under the ice, whether of smooth or turbulent nature. We developed and implemented a parameterization that accounts for flow regime in two sea-ice biogeochemical models. By enhancing nutrient fluxes, turbulence supports higher primary production, resulting in more than double the biomass accumulation.
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