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Aurélie J. Moulin, James N. Moum, and Emily L. Shroyer

currents (±0.5 m) as well as to motion induced by surface gravity waves (±1.0 m). Fig . 3. Simultaneous temperature profiles in the upper ocean from the Chameleon profiler (black) and from the T -chain (blue). Note that three additional CTDs were installed on the T -chain at 8.6, 9.7, and 10.7 m at the above time, which occurred after the time period presented in Fig. 1 . 3. Evolution of T ( z ) in the DWL Much of the DYNAMO record is influenced by freshwater lenses formed by precipitating

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