Vertical structure and temporal evolution of an anticyclonic eddy in the Balearic Sea ( western Mediterranean )

Abstract

[1] An anticyclonic eddy in the Balearic Sea (western Mediterranean) was described using data from a mooring line deployed at the northern slope of Mallorca Island at about 900 m deep. Its surface signature was investigated using sea surface height and sea surface temperature images. The eddy, which lasted around 1 month, modified the thermohaline… (More)

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