Arctic Nutrient Streams Chris, Oliver, Steph, Mick NSIDC greatly simplified cartoon of Arctic through-flow. On time scales of 7-10 years ~1Sv of Pacific water migrates to the sub-Arctic Atlantic. This may provide a pathway for nutrients (esp. Si).
Cross-polar tracer flow Tracer concentration at different depths v time for dye initially injected south of Bering Strait into cs510 Arctic cut-out. Movie ends before tracer reaches Labrador and Greenland Seas. Takes ~5- 10 years to transit.
Global nutrient budgets Ganachaud and Wunsch used WOCE and other cruise data in inverse estimate of nutrient fluxes. southward northward Can we see an appropriate Pac Atl silica flux?
Testing in Arctic simulation Pathways are clearly seen. Shallow, silica rich water enters from Pacific and moves to Atlantic – deepening as it goes. Do budgets look plausible?
Budgets across sections – organic+inorganic Denmark Strait -41kmol/s CAA -11kmol/sIceland basin 14kmol/s Bering 38kmol/s
Inorganic part Denmark Strait -38kmol/sIceland basin 13kmol/sCAA -11kmol/s Bering +28kmol/s
Summary Along with riverine input Pacific water through flow is a supplier of North Atlantic silica. Transports in simulations are within estimated total transports.