Seasonal changes in the circulation of the northern North Sea
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2021, Regional Studies in Marine ScienceWeekly variability of hydrography and transport of northwestern inflows into the northern North Sea
2020, Journal of Marine SystemsCitation Excerpt :The FIC originates to the west of the Fair Isle Gap, the narrow sea passage between the Orkney and Shetland archipelagoes through which the current enters the North Sea (Fig. 1). It comprises a mixture of Atlantic water from the northward-flowing European Shelf Edge Current and low-salinity coastal water from around the complex island chains off the western coast of Scotland that is carried north by the Scottish Coastal Current (Fig. 1; Dooley, 1974; Hill et al., 1997; Inall et al., 2009; Marsh et al., 2017; Turrell et al., 1992). Within the North Sea, the path of the FIC has been traced southward from the Fair Isle Gap to approximately 57.5°N (Dooley, 1974; Turrell et al., 1992).
Terrestrial dissolved organic matter distribution in the North Sea
2018, Science of the Total EnvironmentThermohaline forcing and interannual variability of northwestern inflows into the northern North Sea
2017, Continental Shelf ResearchCitation Excerpt :In turn, this strengthens the horizontal salinity gradient and so increases geostrophic flow. Conversely, they propose that southwesterly winds reduce the inflow of high-salinity Atlantic water and so weaken the horizontal salinity gradient (Turrell et al., 1992). Winther and Johannessen (2006) find that northerly winds lead to upwelling of approximately 0.5 m day−1 around the coast of the Shetland Islands, increasing northwards towards the shelf break.