Closure of Secondary Basins Causes Channel Deepening in Estuaries With Moderate to High Friction
Autor: | Nnafie, A., de Swart, H.E., De Maerschalck, B., Van Oyen, Tomas, van der Vegt, M., van der Wegen, Mick, Sub Physical Oceanography, Coastal dynamics, Fluvial systems and Global change, Proceskunde, Marine and Atmospheric Research |
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Přispěvatelé: | Sub Physical Oceanography, Coastal dynamics, Fluvial systems and Global change, Proceskunde, Marine and Atmospheric Research |
Rok vydání: | 2019 |
Předmět: |
geography
geography.geographical_feature_category 010504 meteorology & atmospheric sciences Sediment Estuary 010502 geochemistry & geophysics 01 natural sciences Geophysics Oceanography Closure (computer programming) General Earth and Planetary Sciences Sediment transport Geology Beach morphodynamics 0105 earth and related environmental sciences Communication channel |
Zdroj: | Geophysical Research Letters, 46. Wiley Online Library |
ISSN: | 1944-8007 0094-8276 |
DOI: | 10.1029/2019gl084444 |
Popis: | Estuaries are often characterized by the presence of secondary basins (side embayments), which affect the estuarine hydrodynamics and sediment dynamics. Many of these basins have disappeared due to land reclamations, which might influence the estuarine morphodynamics. This study addresses how the presence and closure of secondary basins affect the estuarine channel depth using the Delft3D model. Results reveal that channels in estuaries with secondary basins are shallower than those in which these basins are absent, regardless of their location, length, or number. This shallowing is more pronounced for basins that are located at the northern estuarine margin due to the Coriolis force. The shallowing of channels increases if more secondary basins are present. Channels deepen after the closure of secondary basins, resulting from a decrease of the landward directed sediment transport that is driven by tidal asymmetry. Model results apply to estuaries with moderate to high friction. |
Databáze: | OpenAIRE |
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