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Deep-ocean transport and decadal variability inferred from anthropogenic transient tracer observations

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If you have a question about this talk, please contact Prof. John R. Taylor .

The penetration of anthropogenic transient tracers, such as chlorofluorocarbons (CFCs) and sulfur-hexafluoride (SF6), into the oceans represents an opportunity to trace intermediate-to-abyssal water masses as they leave the surface mixed layer and estimate the ventilation rate of the global ocean since 1940. I will present analyses based on four decades of CFCs and SF6 observations to reconstruct global tracer budgets and infer decadal variability of deep ocean circulation and tracer ventilation rates.

This talk is part of the Quantitative Climate and Environmental Science Seminars series.

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Johnson Matthey Lecture Theatre, Department of Chemical Engineering & Biotechnology, Philippa Fawcett Drive, Cambridge CB3 0AS Old Hall, Queens' College (tbc) zoom.us/j/92447982065?pwd=RkhaYkM5VTZPZ3pYSHptUXlRSkppQT09

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