Horizontal patterns of water temperature and salinity in an estuarine tidal channel: Ria de Aveiro |
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Authors: | Nuno Vaz João Miguel Dias Paulo Leitão Inês Martins |
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Institution: | (1) Departamento de Física, Universidade de Aveiro, Campus de Santiago, 3810-193 Aveiro, Portugal;(2) Departamento de Física, Universidade de Aveiro, Campus de Santiago, 3810-193 Aveiro, Portugal;(3) Hidromod, Av. Manuel da Maia, n°36, 3°esq, 1000-201 Lisboa, Portugal;(4) Departamento de Física, Universidade de Aveiro, Campus de Santiago, 3810-193 Aveiro, Portugal |
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Abstract: | This work presents results from two complementary and interconnected approaches to study water temperature and salinity patterns
in an estuarine tidal channel. This channel is one of the four main branches of the Ria de Aveiro, a shallow lagoon located
in the Northwest coast of the Iberian Peninsula. Longitudinal and cross-sectional fields of water temperature and salinity
were determined by spatial interpolation of field measurements. A numerical model (Mohid) was used in a 2D depth-integrated
mode in order to compute water temperature and salinity patterns. The main purpose of this work was to determine the horizontal
patterns of water temperature and salinity in the study area, evaluating the effects of the main forcing factors. The field
results were depth-integrated and compared to numerical model results. These results obtained using extreme tidal and river
runoff forcing, are also presented. The field results reveal that, when the river flow is weak, the tidal intrusion is the
main forcing mechanism, generating saline and thermal fronts which migrate with the neap/spring tidal cycle. When the river
flow increases, the influence of the freshwater extends almost as far as the mouth of the lagoon and vertical stratification
is established. Results of numerical modelling reveal that the implemented model reproduces quite well the observed horizontal
patterns. The model was also used to study the hydrology of the study area under extreme forcing conditions. When the model
is forced with a low river flow (1 m3 s−1) the results confirm that the hydrology is tidally dominated. When the model is forced with a high river flow (1,000 m3 s−1) the hydrology is dominated by freshwater, as would be expected in such an area. |
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Keywords: | Salinity Temperature Transport model Coastal lagoon Ria de Aveiro Espinheiro channel |
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