IMIS | Flanders Marine Institute
 

Flanders Marine Institute

Platform for marine research

IMIS

Publications | Institutes | Persons | Datasets | Projects | Maps
[ report an error in this record ]basket (0): add | show Print this page

Discontinuous Galerkin modeling of the Columbia River's coupled estuary-plume dynamics
Vallaeys, V.; Kärnä, T.; Delandmeter, P.; Lambrechts, J.; Baptista, A.M.; Deleersnijder, E.; Hanert, E. (2018). Discontinuous Galerkin modeling of the Columbia River's coupled estuary-plume dynamics. Ocean Modelling 124: 111-124. https://hdl.handle.net/10.1016/j.ocemod.2018.02.004
In: Ocean Modelling. Elsevier: Oxford. ISSN 1463-5003; e-ISSN 1463-5011, more
Peer reviewed article  

Available in  Authors 

Keywords
    Marine; Brackish water; Fresh water
Author keywords
    Unstructured mesh; Multi-scale model; River-to-ocean continuum; Plumedynamics; Columbia River estuary

Authors  Top 
  • Vallaeys, V., more
  • Kärnä, T., more
  • Delandmeter, P., more
  • Lambrechts, J., more
  • Baptista, A.M.
  • Deleersnijder, E., more
  • Hanert, E., more

Abstract
    The Columbia River (CR) estuary is characterized by high river discharge and strong tides that generate high velocity flows and sharp density gradients. Its dynamics strongly affects the coastal ocean circulation. Tidal straining in turn modulates the stratification in the estuary. Simulating the hydrodynamics of the CR estuary and plume therefore requires a multi-scale model as both shelf and estuarine circulations are coupled. Such a model has to keep numerical dissipation as low as possible in order to correctly represent the plume propagation and the salinity intrusion in the estuary. Here, we show that the 3D baroclinic discontinuous Galerkin finite element model SLIM 3D is able to reproduce the main features of the CR estuary-to-ocean continuum. We introduce new vertical discretization and mode splitting that allow us to model a region characterized by complex bathymetry and sharp density and velocity gradients. Our model takes into account the major forcings, i.e. tides, surface wind stress and river discharge, on a single multi-scale grid. The simulation period covers the end of spring-early summer of 2006, a period of high river flow and strong changes in the wind regime. SLIM 3D is validated with in-situ data on the shelf and at multiple locations in the estuary and compared with an operational implementation of SELFE. The model skill in the estuary and on the shelf indicate that SLIM 3D is able to reproduce the key processes driving the river plume dynamics, such as the occurrence of bidirectional plumes or reversals of the inner shelf coastal currents.

All data in the Integrated Marine Information System (IMIS) is subject to the VLIZ privacy policy Top | Authors