Shelf-basin exchange times of Arctic surface waters estimated from 228Th/228Ra disequilibrium

• Published in: Journal of Geophysical Research: Oceans
• Main Authors: Rutgers v. d. Loeff, Michiel, Cai, Pinghe, Stimac, Ingrid, Bauch, D., Hanfland, Claudia, Roeske, Tobias, Moran, S. B.
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: 2012
• Subjects: Arctic; laptev; Lomonosov Ridge
• Online Access: https://epic.awi.de/id/eprint/24715/; https://epic.awi.de/id/eprint/24715/1/RvdLetalThRaArcticJGRPostprint.pdf; https://hdl.handle.net/10013/epic.39149; https://hdl.handle.net/10013/epic.39149.d001

The Trans Polar Drift is strongly enriched in 228Ra accumulated on the wide Arctic shelves with subsequent rapid off-shore transport. We present new data of Polarstern expeditions to the central Arctic and to the Kara and Laptev Seas. Because 226Ra activities in Pacific waters are 30% higher than in Atlantic waters, we correct 226Ra for the Pacific admixture when normalizing 228Ra with 226Ra. The use of 228Ra decay as age marker critically depends on the constancy in space and time of the source activity, a condition that has not yet adequately been tested. While 228Ra decays during transit over the central Basin, ingrowth of 228Th could provide an alternative age marker. The high 228Th/228Ra activity ratio (AR=0.8 – 1.0) in the central basins is incompatible with a mixing model based on horizontal eddy diffusion. An advective model predicts that 228Th grows to an equilibrium AR, the value of which depends on the scavenging regime. The low AR over the Lomonosov Ridge (AR=0.5) can be due to either rapid transport (minimum age without scavenging 1.1 year) or enhanced scavenging. Suspended particulate matter (SPM) load (derived from beam transmission and particulate 234Th) and total 234Th depletion data show that scavenging, although extremely low in the central Arctic, is enhanced over the Lomonosov Ridge, making an age of 3 yr more likely. The combined data of 228Ra decay and 228Th ingrowth confirm the existence of a recirculating gyre in the surface water of the eastern Eurasian Basin with a river water residence time of at least 3 years.