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- W2328005454 abstract "Measurements of water properties in the Great South Channel (GSC) made on 35 surveys between 1977 and 1985 indicate an intrusion of high salinity water in the autumn of most years. The intrusion represents an influx of slope water. It is most evident near bottom, but high salinity values are found throughout the water column. In some years the intrusion can be traced through the channel to the north side of Georges Bank. Larvae of offshore, warm-water fish species found in the high salinity intrusion support reports that the presence of these larvae is associated with an influx of slope water through the channel. The influx is likely to be associated with the seasonal shelfward movement of the shelf/slope front during the autumn. While the extent of the influx may be modified by Gulf Stream rings located south of the channel region, the phenomenon does not appear to be caused by rings. The influx of slope water across the shelf and to GSC suggests a seasonal reduction in the transport of Georges Bank water westward past Nantucket Shoals." @default.
- W2328005454 created "2016-06-24" @default.
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- W2328005454 date "1989-12-01" @default.
- W2328005454 modified "2023-09-26" @default.
- W2328005454 title "Slope Water Intrusion to the Great South Channel During Autumn, 1977-85" @default.
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- W2328005454 doi "https://doi.org/10.2960/j.v9.a8" @default.
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