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- W2005056759 abstract "Observations from a four-year current meter mooring at 28°44′N, 13°28′W in the Lanzarote passage are used to describe the transport variability of the Eastern Boundary Current of the North Atlantic Subtropical Gyre. Three different water masses are found in the passage: North Atlantic Central Water in the upper levels (roughly 0–600m), Antarctic Intermediate Water (roughly 600–1100m) and Mediterranean Water in the layer above the bottom at 1300m. The mean southward transport of NACW is −0.8±1.1Sv (1Sv=109kgs−1) which is the transport of the easternmost branch of the Canary Current. Fluctuations of NACW transport are large, ranging from −3.4Sv southward to 1.7Sv northward. Every autumn a consistent northward transport is observed, which may be related with the eastern boundary upwelling dynamics. The mean transports of AAIW and MW are 0.1±0.4Sv northward and −0.05±0.09Sv southward, respectively. Fluctuations of transport of AAIW and MW are large, from 1.0 to −1.0Sv and from −0.32 to 0.23Sv, respectively. Thus, the mass transports for each water mass show a high standard deviation of comparable magnitude to the mean. This highlights the importance of the temporal variability of the currents in this passage. A remarkable feature of our observations is that the mean transports of NACW and AAIW during an El Niño event are significantly different." @default.
- W2005056759 created "2016-06-24" @default.
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- W2005056759 date "2003-02-01" @default.
- W2005056759 modified "2023-09-27" @default.
- W2005056759 title "Transport variability in the Lanzarote passage (eastern boundary current of the North Atlantic subtropical Gyre)" @default.
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- W2005056759 doi "https://doi.org/10.1016/s0967-0637(02)00163-2" @default.
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