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How does the Southern Ocean “Great Calcite Belt” emerge? Insights from CESM-MARBL

Coccolithophores, unicellular calcifying phytoplankton, grow in a region spanning the entire Southern Ocean termed the “Great Calcite Belt” (GCB). Particulate inorganic carbon (PIC) is generated through the process of coccolithophore calcification, and the GCB is thought to host over a quarter of globally suspended PIC. Sensitive to changes in temperature and ocean alkalinity, coccolithophore growth…

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Coccolithophore growth dynamics in the Pacific Sector of the Southern Ocean

In our new paper “Environmental Drivers of Coccolithophore Growth in the Pacific Sector of the Southern Ocean” we use both observations (shipboard and remote sensing) in combinations with simple growth models (parameterized using CESM/MARBL) to understand what are the major driving factors controlling calcification in the Subantarctic Zone, particularly far from any sedimentary sources. This…

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The local biogeochemical impacts of Greenland subglacial discharge

Much of Greenland runoff is delivered to the coastal ocean at marine-terminating glaciers, potentially hundreds of meters below the sea surface. The resulting turbulent buoyant plumes can entrain nurtrient-rich deeper waters, potentially delivering these nutrients to the upper water column which can support elevated primary productivity. The importance of this buoyant plume-productivity effect around Greenland…

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Buoyant Plume Dynamics Across Greenland

Check out our new paper characterizing buoyant plume dynamics across Greenland, led by Donald Slater “Characteristic depths, fluxes, and timescales for Greenland’s tidewater glacier fjords from subglacial discharge-driven upwelling during summer”. Watch Donald’s IGS seminar on this work here. (Article PDF)  

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