Inversions Beneath the thermocline in the north-western Mediterranean

descriptionPublicationkeyboard_double_arrow_right Article , Other literature type 01 Jul 1973 English Publisher:Springer Science and Business Media LLCJournal:Deutsche Hydrographische Zeitschrift, volume 26, pages 145-154 (issn: 0012-0308, eissn: 1616-7228,

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Authors: Ekkehard Mittelstaedt; Klaus Huber;

doi: 10.1007/bf02232608

Inversions Beneath the thermocline in the north-western Mediterranean

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Abstract

Vertical temperature traces in the north-western Mediteranean show remarkably leafy structures at depths between 100 m and 300 m. The individual layers are stable over several days. Their horizontal extension is larger than 20 nm. The thickness amounts to 25–50 m. It is suggested that these interleavings of slightly different water masses are due to lateral mixing processes in the vicinity of the working area.

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