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- W2023005003 abstract "Hydrographic observations in 1983 and current meter data reveal a subsurface eddy at 47°N, 20°W. Its diameter is about 75 km. In the center an accumulation of water of Mediterranean origin is found which, at 1500 dbar, is 1.5°C warmer and 0.3 saltier than the surrounding water. The water mass anomaly extends down to 2400 dbar. At mid-depth of the eddy (1700–2100 dbar), a high percentage of a Turner angle >71.6° indicates the possibility for strong salt fingering. Geostrophic velocities referred to 4000 dbar indicate a cyclonic movement. A relative velocity maximum of more than 10 cm s−1 lies at 1750 dbar; true maximal velocities at 1570 m are 15 cm s−1 according to current meter records. In combination with the hydrographic data, the Eulerian measurements document a movement of the eddy westward with a phase velocity of 1.1–5.8 cm s−1. It is concluded that this is a deep cyclonic counterpart of the anticyclonic “Meddies” that usually are found south of the Mediterranean Water tongue in the northeast Atlantic. A first review of velocity and temperature recordic reveals, since 1972, at least seven deep cyclonic eddies in the northeast Atlantic between 40° and 50°N." @default.
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- W2023005003 date "1989-10-01" @default.
- W2023005003 modified "2023-09-27" @default.
- W2023005003 title "A deep saline cyclonic eddy in the west european basin" @default.
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- W2023005003 doi "https://doi.org/10.1016/0198-0149(89)90057-5" @default.
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