Arctic Ocean Boundary Current Modeling With Transient Tracers
Arctic Ocean Boundary Current Modeling With Transient Tracers
Type:
Parallel
Time:
16 March 2010 - 3:30pm Abigail R. Mauldin1, Peter Schlosser2, Robert Newton3, William M Smethie4
1Earth and Environmental Sciences, Columbia University, Lamont Doherty Earth Observatory-Comer Bld., 61 Route 9W, Palisades, NY, 10964, USA, spieler [at] ldeo [dot] columbia [dot] edu
2Earth and Environmental Sciences, Columbia University, Lamont Doherty Earth Observatory-Comer Bld., 61 Route 9W, Palisades, NY, 10964, USA, schlosser [at] ldeo [dot] columbia [dot] edu
3Lamont Doherty Earth Observatory, Palisades, NY, USA, bnewton [at] ldeo [dot] columbia [dot] edu
4Lamont Doherty Earth Observatory, Palisades, NY, USA, bsmeth [at] ldeo [dot] columbia [dot] edu
The Arctic Ocean boundary current transports Atlantic-origin waters cyclonically for thousands of kilometers around the perimeter of the Eurasian and Canadian Basins, propagating temperature and salinity anomalies originating in the Barents and Greenland Seas into the Arctic Ocean. Transient tracer data collected at 22 locations provide a basin-wide, time-integrated view of the boundary current. We use these data to constrain a transit-time-distribution model of the Barents Sea Branch Water in the boundary current. The modeled mean velocity of the current is 2.5 ±0.5 cm s-1 and the mixing timescale between the boundary and the interior is 5-10 years.