HIGHLIGHTS
SUMMARY
Some of the key events that directly influenced the measurements are outlined below, providing additional information that helps to interpret the data set. Microstructure sampling operations were continued during the course of the wind event, providing first-hand observations of the ice-covered upper ocean under the influence of strong winds and in the proximity of a newly forming lead, e_g a deepening of the surface mixed layer. In the energetic surface layer, above 20 m depth, dissipation rates highly depend on the surface forcing, e_g the ice drift speed, and range from 10 . . .
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