The ocean mixed-layer under Southern Ocean sea-ice: Seasonal cycle and forcing

• Published in: Journal of Geophysical Research: Oceans
• Main Authors: Pellichero, Violaine, Sallée, Jean-Baptiste, Schmidtko, Sunke, Roquet, Fabien, Charrassin, Jean-Benoît
• Format: Article in Journal/Newspaper
• Language: English
• Published: AGU (American Geophysical Union) 2017
• Subjects: Southern Ocean; Elephant Seal; Sea ice
• Online Access: https://oceanrep.geomar.de/id/eprint/34943/; https://oceanrep.geomar.de/id/eprint/34943/1/jgrc22039.pdf; https://doi.org/10.1002/2016JC011970

The oceanic mixed-layer is the gateway for the exchanges between the atmosphere and the ocean; in this layer all hydrographic ocean properties are set for months to millennia. A vast area of the Southern Ocean is seasonally capped by sea-ice, which alters the characteristics of the ocean mixed-layer. The interaction between the ocean mixed-layer and sea-ice plays a key role for water-mass transformation, the carbon cycle, sea-ice dynamics, and ultimately for the climate as a whole. However, the structure and characteristics of the under-ice mixed-layer are poorly understood due to the sparseness of in-situ observations and measurements. In this study, we combine distinct sources of observations to overcome this lack in our understanding of the Polar Regions. Working with Elephant Seal-derived observations, ship-based and Argo float observations, we describe the seasonal cycle of the ocean mixed-layer characteristics and stability of the ocean mixed-layer over the Southern Ocean and specifically under sea-ice. Mixed-layer heat and freshwater budgets are used to investigate the main forcing mechanisms of the mixed-layer seasonal cycle. The seasonal variability of sea surface salinity and temperature are primarily driven by surface processes, dominated by sea-ice freshwater flux for the salt budget, and by air-sea flux for the heat budget. Ekman advection, vertical diffusivity and vertical entrainment play only secondary roles.Our results suggest that changes in regional sea-ice distribution and annual duration, as currently observed, widely affect the buoyancy budget of the underlying mixed-layer, and impact large-scale water-mass formation and transformation with far reaching consequences for ocean ventilation.