Understanding Circulation Processes in the Arctic and sub-Arctic Regions Using a Combination of Anthropogenic Chemical Tracers
Abstract:
Here we will present the results of a combination of anthropogenic radionuclides (i.e. 129I, 236U, 233U, 14C) measured in the Arctic Ocean (including sub-polar North Atlantic) during several expeditions that took place over the last 6 years. The distribution of 129I and 236U measured in 2015 are a consequence of the anticyclonic atmospheric regime, which shifted the Pacific-Atlantic front towards the North Pole resulting in a weaker boundary current in the Beaufort Sea. The combination of 129I and 236U in a dual tracer approach will be used to revisit the tracer ages of Atlantic waters throughout their transit in the Arctic Ocean (embracing both the Eurasian and Canada basins) and back to the Atlantic Ocean. Additional data on 129I, 236U and 14C in the Fram Strait and sub-polar North Atlantic will be also discussed in the context of the previous results. Finally, the combination of the long-lived 129I and 236U with CFCs and SF6 to extract TTD will be presented as a tool to study parameters associated with mixing and advection.
In this study we therefore highlight the importance of studying the combination of several transient tracers with different historical and regional source inputs, in a holistic approach.