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Beryllium-7 as a tracer of surface water subduction and mixed-layer history

Kadko, David (University of Miami, RSMAS/MAC, 4600 Rickenbacker Causeway, Miami, FL 33149, USA ); Olson, Donald ( University of Miami, RSMAS/MAC, 4600 Rickenbacker Causeway, Miami, FL 33149, USA );
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    Abstract Beryllium-7 is a cosmic-ray-produced radioactive nuclide (half-life 53.3 days) that is deposited upon the ocean surface by rainfall. Beryllium-7 profiles were collected and analyzed in May 1991 and March 1992 as part of the ONR SUBDUCTION program. The 7 Be activities were homogeneous in the mixed layer and ranged approximately from 100 to 200 dpm/ 1000 1. The activities dropped off rapidly in the upper thermocline. The 7 Be profiles were modeled using a simple seasonal progression of mixed-layer depth, indicating that seasonal changes in the mixed-layer depth control the main features of the profile. The observed temperature, salinity and 7 Be profiles from the May 1991 cruise show warm salinity maxima associated with a layer of high 7 Be penetrating into the upper seasonal thermocline. The high 7 Be concentration suggests that these waters were in relatively thin mixed layers within, approximately, the past month. The model results indicate that in late spring both salinity and 7 Be can respond to a shoaling mixed layer on a similar timescale leading to the observed anomalies in the subducted water layer.


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