Abstract:On the basis of in-situ hydro-physical one year long time series, acquired in June, 2016-July, 2017, in the North Atlantic Subpolar Gyre, along with the use of up to date satellite data, detailes of long term variability of surface and near-bottom flows over Reykjanes Ridge flanks and near the Hatton Bank (Rockall Plateau) are presented.
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