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- W1970996969 abstract "Deepwater turnover time is an important variable for coastal management because it regulates fluxes of nutrients and oxygen consumption. The aim of this study was to develop a model to predict mean or characteristic deepwater turnover time in nontidal Baltic areas for the summer period. It is hypothesized that morphometry governs the exchange of deep water. Empirical data were collected during summer from 15 relatively small areas with varying topography. Deepwater turnover time was determined from the dispersal of a fluorescent dye. Statistical relationships between deepwater turnover time and morphometric parameters, determined using a digital technique, were calculated using multivariate methods. The results show that 82% of the variation in deepwater turnover time among the areas can be statistically explained by the mean filter factor, the topographic openness, and the mean slope. The mean filter factor describes how an archipelago acts as an energy filter, and openness describes the exposure of the coastal area. Resume : La durOe du turnover en eaux profondes est une importante variable ‡ considOrer dans les plans diamOnagement des secteurs cUtiers parce que ce phOnomne rOgule les flux de nutriments et la consommation dioxygne. Cette Otude a pour but la mise au point diun modle pour prOvoir la durOe du turnover en eaux profondes moyenne ou caractOristique estivale dans des secteurs de la mer Baltique qui ne sont pas soumis aux marOes. Les auteurs ont pris comme hypothse que la morphomOtrie gouverne les Ochanges dieau profonde. Ils ont recueilli des donnOes empiriques au cours diun OtO dans 15 secteurs relativement petits et ‡ la topographie variable. La durOe du turnover en eaux profondes a OtO dOterminOe par la dispersion diun colorant fluorescent. Au moyen de mOthodes multivariOes, ils ont calculO les relations statistiques entre la durOe du turnover en eaux profondes et des paramtres morphomOtriques, quiils ont dOterminOs par une technique numOrique. Les rOsultats montrent que 82% de la variance de la durOe du turnover en eaux profondes entre les secteurs siexplique statistiquement par le coefficient moyen diattOnuation, la topographie ouverte et la pente moyenne. Le coefficient moyen diattOnuation dOcrit de quelle faAon un archipel agit comme un filtre de liOnergie et la topographie ouverte dOcrit liexposition des secteurs cUtiers. (Traduit par la ROdaction)" @default.
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- W1970996969 date "1996-06-01" @default.
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- W1970996969 title "A simple empirical model to predict deepwater turnover time in coastal waters" @default.
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- W1970996969 doi "https://doi.org/10.1139/f96-048" @default.
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