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• W2074570737 abstract "Abstract A mathematical model of the Himmerfja¨rd estuary, divided into four basins, has been formulated and validated against measured data for 1986. The structure of each sub-basin is assumed to be horizontally homogeneous with vertical mean velocities based upon in- and outflows from adjacent basins and freshwater supply to each basin. The horizontal water exchange is formulated as a quasi-stationary Bernoulli flow, driven by horizontal pressure gradients over the sounds and instantaneously interleaved at a neutral buoyancy level. The salinity and temperature profiles measured outside the mouth of the estuary serve as forcing, as do the water level changes, the freshwater run-off and the local wind. Inherent in the model assumptions of the horizontal exchange over the sounds is that only a fraction, α, of the pressure gradient is used to accelerate each stratum. Variation of the α-value shows that the best statistical fit is found for α = 0.15 when compared with water exchange estimates based on measurements in one of the internal sounds for almost an entire month. Using this α-value, in combination with standard mixing parameters and hypsographical data, the model satisfactorily captures the major features of the salinity and temperature profiles development for the year 1986. This is substantiated by statistical analysis of the salinity profiles in the sub-basins for which different measures of similarity between simulated and measured data give the best fit for the same α-value as above." @default.
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• W2074570737 date "1992-09-01" @default.
• W2074570737 modified "2023-09-27" @default.
• W2074570737 title "Water exchange and density structure in a multi-basin estuary" @default.
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• W2074570737 doi "https://doi.org/10.1016/0278-4343(92)90013-a" @default.
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