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- W2040378250 abstract "Bottom nepheloid layers (BNL) are well developed on the west slope of Porcupine Bank, particularly in a narrow zone on the slope lying between the 400 and 600 m isobaths. However, these layers may become detached and spread along isopycnal surfaces to form intermediate nepheloid layers (INL) further off- and along-slope. Vertical sections of properties normal to the slope show that the main zone of BNL formation is marked by a doming of temperature and density isopleths and by a ‘chimney’ in salinity in the overlying watercolumn. The detailed hydrographic structure, however, is one of individually mixed but discrete layers in T, S and nephels suggesting boundary mixing followed by detachment, lateral injection and hence interleaving of layers. Plots of particle volume vs size within these turbid plumes show a persistent peak at 13.5 μm: subsidiary peaks at larger particle diameters, found close to the bed, consist of aggregated smaller material. The layers are believed to be formed by bottom erosion under internal tides and waves. Under northerly (long-slope) winds the 9°C isotherm is drawn up the slope, the density gradient steepens close to the bed and the slope of the characteristic for M2 tidal frequency, α = [(σ2 − ƒ2)12/(N2 − σ2)12], comes close to the bottom sf slope β at the poiint where maximum intensity BNL's are observed. Temperature spectra under these conditions show increased total energy and it is thought that high-frequency internal waves also propagate along the sharpened density surface to impinge on the slope." @default.
- W2040378250 created "2016-06-24" @default.
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- W2040378250 date "1986-06-01" @default.
- W2040378250 modified "2023-10-16" @default.
- W2040378250 title "Nepheloid layers on the continental slope west of Porcupine Bank" @default.
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- W2040378250 doi "https://doi.org/10.1016/0198-0149(86)90089-0" @default.
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