ETD

Archivio digitale delle tesi discusse presso l'Università di Pisa

Tesi etd-03272015-131318


Tipo di tesi
Tesi di laurea magistrale
Autore
NOVI, LYUBA
URN
etd-03272015-131318
Titolo
Sensitivity of the mesoscale quasi-geostrophic turbulence to the numerical advection scheme: application to an Antarctic Ocean channel dynamics
Dipartimento
INGEGNERIA CIVILE E INDUSTRIALE
Corso di studi
INGEGNERIA AEROSPAZIALE
Relatori
relatore Prof. Salvetti, Maria Vittoria
Parole chiave
  • turbulence
  • cfd
  • applied mathematics.
  • fluid dynamics
Data inizio appello
28/04/2015
Consultabilità
Completa
Riassunto
The interactions of mesoscale eddies cause the potential enstrophy (the variance
of potential vorticity) to be transferred toward small scales. To prevent
a pileup of potential enstrophy at the grid size scale, models should dissipate
the enstrophy. This can be done explicitly or implicitly via the the advection
scheme. We explore the second choice and compare a set of schemes
(2nd order MUSCL type, the ROMS one and two 5th order ones including a
WENO). The comparison is done with a 3D QG model in a forced-dissipated
turbulent regime. We assess the behavior with resolution. We nd a significant
impact of the advection scheme on the turbulence, likely due to the
inverse cascade of kinetic energy. We are able to diagnose the spectral signature
of the implicit dissipation for each scheme. This reveals and explains
why the eddy kinetic energy can so dramatically di er from one scheme to
the other. Statistically convergence is also assessed, as well as robustness
with c
. In conclusion this work is aimed at exploring the e ects of implicit
dissipation in the eddy resolving regime.
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