A comparison of the motions of surface drifters with offshore wind properties in the Gulf of Finland, the Baltic Sea
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Properties of wind and surface drift compared in the Gulf of Finland for 2011–2013.

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Surface layer drift in most cases governed by Ekman transport.

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Rapid across-gulf transport may occur on a time scale of 6–12 days.

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In weak wind conditions currents in a deeper layer dominate the drift.

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