Výsledky vyhledávání - "De swart, H. E."

TIDAL INLET EXPANSION FROM SEA LEVEL RISE

Autor: Nienhuis, J. H., Portos-Amill, L., De swart, H. E., Roebeling, M.r.w., Wang, Ping, Royer, Elizabeth, Rosati, Julie D

Publikováno v: Proceedings Coastal Sediments 2023, 71-76
STARTPAGE=71;ENDPAGE=76;TITLE=Proceedings Coastal Sediments 2023

Tidal inlets are expected to expand as sea-level rise accelerates, and, in extreme cases, might fully drown barrier islands. Here we report on field observations and model predictions of tidal inlet expansion. Field observations show that many inlets

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f0f71d3cce41432d3e403543d797d6b1
https://doi.org/10.1142/9789811275135_0007

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Sensitivity of modeled tracer motion in tidal areas to numerics and to non-Hamiltonian perturbations

Autor: de Swart, H. E., van der Wal, S. T., Frank, J. E.

This study focuses on the motion of passive tracers induced by the joint action of tidal and residual currents in shallow seas with an irregular bottom topography. Interest in this problem has rapidly increased in recent years, because of the detecti

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=od_______101::cd06bf79c024f9b846ee5ba269d4cc81
https://dspace.library.uu.nl/handle/1874/422925

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Akademický článek

An Idealized Model and Systematic Process Study of Oxygen Depletion in Highly Turbid Estuaries

Autor: Talke, S. A., de Swart, H. E., de Jonge, V. N.

Publikováno v: Estuaries and Coasts, 2009 Jul 01. 32(4), 602-620.

Externí odkaz: https://www.jstor.org/stable/40663569

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On the mechanism behind the shift of the turbidity maximum zone in response to reclamations in the Yangtze (Changjiang) Estuary, China

Autor: Teng, Lizhi, Cheng, Heqin, de Swart, H. E., Dong, Ping, Li, Zhanhai, Li, Jiufa, Wang, Yajun, Sub Physical Oceanography, Marine and Atmospheric Research

Publikováno v: Marine Geology, 440, 1. Elsevier
MARINE GEOLOGY

Reclamation in estuaries can greatly change the channel geometry and hydrodynamic conditions and these changes may have significant impacts on spatial and temporal distribution of the turbidity maximum zone. This study focuses on the effects of a lar

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::38f27c4b145041855542a6e0055e403f
https://dspace.library.uu.nl/handle/1874/413350

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Modelling the response of a double-barred sandy beach system to time-varying wave angles

Autor: Nnafie, A., Driessen, A. S., de Swart, H. E., Price, T. D.

Sandy beaches typically have one or more shore-parallel bars with superimposed smaller-scale three-dimensional (3D) bars. Knowledge of their morphodynamic behaviour under more realistic wave conditions is limited. This study investigates the response

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=od_______101::e91697e76e076d8087c77d79e3cf3fcc
https://dspace.library.uu.nl/handle/1874/413352

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Long-term morphodynamics of a coupled shelf-shoreline system forced by waves and tides, a model approach

Autor: Nnafie, A., de Swart, H. E., Falqués, A., Calvete, D., Afd Marine and Atmospheric Research, Sub Physical Oceanography, Dep Natuurkunde, Marine and Atmospheric Research

Publikováno v: UPCommons. Portal del coneixement obert de la UPC
Universitat Politècnica de Catalunya (UPC)
Journal of Geophysical Research: Earth Surface, 126(12), 1. Wiley

Sand ridges, with length scales of several km, are prominent features of the seafloor landscape of many sandy continental shelves. Knowledge about the extent to which these ridges influence the large-scale (i.e., decadal and kilometer scales) morphod

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d4c6f5b391157f6122e70d8abad13d64
http://hdl.handle.net/2117/358860

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Tidal sand ridges on the shelf: A numerical study of their natural morphodynamic evolution and response to interventions

Autor: Nnafie, A., Wolf, T. B.J., de Swart, H. E., Afd Marine and Atmospheric Research, Sub Physical Oceanography, Marine and Atmospheric Research

Publikováno v: Continental Shelf Research, 205. Elsevier Limited

Tidal sand ridges are large-scale bottom features that occur on continental shelves with strong tidal currents and abundance of sand. These ridges have longshore spacings of several kilometres, heights of tens of metres, they evolve on centennial tim

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f646de366a9fd8d3db7596f123f8086d
https://doi.org/10.1016/j.csr.2020.104195

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Estuarine residual flow induced by eddy viscosity-shear covariance: Dependence on axial bottom slope, tidal intensity and constituents

Autor: Chen, W., de Swart, H. E., Helmholtz Institute, Sub Physical Oceanography

Publikováno v: Continental Shelf Research, 167, 1. Elsevier Limited

Residual flow generated by Eddy viscosity-Shear Covariance (ESCO) in a narrow estuary is investigated with a numerical model. New aspects concern the dependence of the spatial structure of ESCO flow on (1) longitudinal depth variation for fixed semi-

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::244a8bfa48f16c90f50caeb0c0c5dbef
https://dspace.library.uu.nl/handle/1874/371799

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