Cristin-resultat-ID: 1699524
Sist endret: 13. mars 2020, 16:40
NVI-rapporteringsår: 2019
Resultat
Vitenskapelig artikkel
2019

Numerical analysis of boundary conditions in a Lagrangian particle model for vertical mixing, transport and surfacing of buoyant particles in the water column

Bidragsytere:
  • Tor Nordam
  • Ruben Kristiansen
  • Raymond Nepstad og
  • Johannes Röhrs

Tidsskrift

Ocean Modelling
ISSN 1463-5003
e-ISSN 1463-5011
NVI-nivå 1

Om resultatet

Vitenskapelig artikkel
Publiseringsår: 2019
Publisert online: 2019
Trykket: 2019
Volum: 136
Sider: 107 - 119
Open Access

Importkilder

Scopus-ID: 2-s2.0-85064313600

Beskrivelse Beskrivelse

Tittel

Numerical analysis of boundary conditions in a Lagrangian particle model for vertical mixing, transport and surfacing of buoyant particles in the water column

Sammendrag

Lagrangian particle models are used for many applications in the ocean sciences, including transport modelling of oil spills, fish eggs and larvae, plastics, and sediment particles. In the context of oil spill modelling, there are numerous papers discussing entrainment of surface oil by breaking waves. However, for the opposite process, i.e., droplets reaching the surface and joining the surface slick, we have found no discussion in the literature of the exact steps involved. Given the wide use of particle-based models in oil spill modelling, it is important to establish a consistent recipe for treating the surface boundary. We investigate a Lagrangian particle model for the vertical transport, surfacing and resuspension of buoyant material in the water column. By modifying the behaviour at the surface boundary, the model can be applied to materials such as oil droplets, that form a surface slick, and hence see the surface as an absorbing boundary, and to particles that do not form a surface slick, such as fish eggs and microplastics. For slick-forming materials, we also consider resuspension from the surface slick, (e.g., entrainment of surface oil by breaking waves). While we restrict our attention to positively buoyant materials, the model is equally applicable to the settling of negatively buoyant particles, such as sediment grains and marine snow. We consider three case studies, each designed to allow a detailed and direct comparison of the Lagrangian model to an Eulerian model based on numerical solution of the advection-diffusion-reaction equation. We demonstrate that the two models give the same results when the boundary at the surface is treated correctly.

Bidragsytere

Tor Nordam

  • Tilknyttet:
    Forfatter
    ved Institutt for fysikk ved Norges teknisk-naturvitenskapelige universitet
  • Tilknyttet:
    Forfatter
    ved Klima og miljø ved SINTEF Ocean

Ruben Kristiansen

  • Tilknyttet:
    Forfatter
    ved Institutt for fysikk ved Norges teknisk-naturvitenskapelige universitet

Raymond Nepstad

  • Tilknyttet:
    Forfatter
    ved Klima og miljø ved SINTEF Ocean

Johannes Röhrs

  • Tilknyttet:
    Forfatter
    ved Meteorologisk institutt
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