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dc.contributor.authorRutgers van der Loeff, Michiel M.  Concept link
dc.contributor.authorKipp, Lauren  Concept link
dc.contributor.authorCharette, Matthew A.  Concept link
dc.contributor.authorMoore, Willard S.  Concept link
dc.contributor.authorBlack, Erin E.  Concept link
dc.contributor.authorStimac, Ingrid  Concept link
dc.contributor.authorCharkin, Alexander  Concept link
dc.contributor.authorBauch, Dorothea  Concept link
dc.contributor.authorValk, Ole  Concept link
dc.contributor.authorKarcher, Michael  Concept link
dc.contributor.authorKrumpen, Thomas  Concept link
dc.contributor.authorCasacuberta, Nuria  Concept link
dc.contributor.authorSmethie, William M.  Concept link
dc.contributor.authorRember, Robert  Concept link
dc.identifier.citationJournal of Geophysical Research: Oceans 123 (2018): 4853-4873en_US
dc.description© The Author(s), 2018. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Journal of Geophysical Research: Oceans 123 (2018): 4853-4873, doi:10.1029/2018JC013888.en_US
dc.description.abstractThe first full transarctic section of 228Ra in surface waters measured during GEOTRACES cruises PS94 and HLY1502 (2015) shows a consistent distribution with maximum activities in the transpolar drift. Activities in the central Arctic have increased from 2007 through 2011 to 2015. The increased 228Ra input is attributed to stronger wave action on shelves resulting from a longer ice‐free season. A concomitant decrease in the 228Th/228Ra ratio likely results from more rapid transit of surface waters depleted in 228Th by scavenging over the shelf. The 228Ra activities observed in intermediate waters (<1,500 m) in the Amundsen Basin are explained by ventilation with shelf water on a time scale of about 15–18 years, in good agreement with estimates based on SF6 and 129I/236U. The 228Th excess below the mixed layer up to 1,500 m depth can complement 234Th and 210Po as tracers of export production, after correction for the inherent excess resulting from the similarity of 228Ra and 228Th decay times. We show with a Th/Ra profile model that the 228Th/228Ra ratio below 1,500 m is inappropriate for this purpose because it is a delicate balance between horizontal supply of 228Ra and vertical flux of particulate 228Th. The accumulation of 226Ra in the deep Makarov Basin is not associated with an accumulation of Ba and can therefore be attributed to supply from decay of 230Th in the bottom sediment. We estimate a ventilation time of 480 years for the deep Makarov‐Canada Basin, in good agreement with previous estimates using other tracers.en_US
dc.description.sponsorshipU.S. National Science Foundation Grant Numbers: OCE‐1458305, OCE‐1458424; US NSF Grant Number: OCE‐1433922en_US
dc.publisherJohn Wiley & Sonsen_US
dc.rightsAttribution-NonCommercial-NoDerivatives 4.0 International*
dc.subjectArctic Oceanen_US
dc.subjectTranspolar driften_US
dc.titleRadium isotopes across the Arctic Ocean show time scales of water mass ventilation and increasing shelf inputsen_US

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Except where otherwise noted, this item's license is described as Attribution-NonCommercial-NoDerivatives 4.0 International