Numerical simulations of baroclinic driven flows in a thermally driven rotating annulus using the immersed boundary method

We present results of numerical simulations of baroclinic driven flows in the thermally driven rotating annulus using the immersed boundary method for modeling of the boundary conditions. The Navier-Stokes equations in the Boussinesq approximation are solved in the Eulerian flux-form advection schem...

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Main Authors: Thomas von Larcher, Andreas Dörnbrack
Format: Article
Language:English
Published: Borntraeger 2015-01-01
Series:Meteorologische Zeitschrift
Subjects:
Online Access:http://dx.doi.org/10.1127/metz/2014/0609
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spelling doaj-d8d98cb5a80d48a2904f57ae6f420edb2020-11-24T23:18:29ZengBorntraegerMeteorologische Zeitschrift0941-29482015-01-0123659961010.1127/metz/2014/060984460Numerical simulations of baroclinic driven flows in a thermally driven rotating annulus using the immersed boundary methodThomas von LarcherAndreas DörnbrackWe present results of numerical simulations of baroclinic driven flows in the thermally driven rotating annulus using the immersed boundary method for modeling of the boundary conditions. The Navier-Stokes equations in the Boussinesq approximation are solved in the Eulerian flux-form advection scheme with the geophysical flow solver EULAG as numerical framework. We test our approach against results of an appropriate laboratory experiment with water as working fluid and directly aim at the wavy flow regime where complex flows and regular wave patterns are generally observed but where centrifugal effects and turbulence is of minor importance. Multivariate statistical methods are used for analyzing time series of computed temperature data. We, here, present the outcome of the time series data analysis at particular parameter points, and specifically analyze a complex wave-wave interaction, and, secondly, a wave mode switch where the azimuthal wave number changes to the next higher one. The numerical results are highly consistent with the experimental observations. That encourage us to focus on our actual goal as the next step, that is the irregular flow regime found at large rotation rates where the centrifugal force has an increasing effect on flow states and where multiple scale flows are generally observed.http://dx.doi.org/10.1127/metz/2014/0609baroclinic driven flowsthermally driven rotating annulusnumerical experimentsimmersed boundary methodcomplex flow regimesmultivariate time series analysis
collection DOAJ
language English
format Article
sources DOAJ
author Thomas von Larcher
Andreas Dörnbrack
spellingShingle Thomas von Larcher
Andreas Dörnbrack
Numerical simulations of baroclinic driven flows in a thermally driven rotating annulus using the immersed boundary method
Meteorologische Zeitschrift
baroclinic driven flows
thermally driven rotating annulus
numerical experiments
immersed boundary method
complex flow regimes
multivariate time series analysis
author_facet Thomas von Larcher
Andreas Dörnbrack
author_sort Thomas von Larcher
title Numerical simulations of baroclinic driven flows in a thermally driven rotating annulus using the immersed boundary method
title_short Numerical simulations of baroclinic driven flows in a thermally driven rotating annulus using the immersed boundary method
title_full Numerical simulations of baroclinic driven flows in a thermally driven rotating annulus using the immersed boundary method
title_fullStr Numerical simulations of baroclinic driven flows in a thermally driven rotating annulus using the immersed boundary method
title_full_unstemmed Numerical simulations of baroclinic driven flows in a thermally driven rotating annulus using the immersed boundary method
title_sort numerical simulations of baroclinic driven flows in a thermally driven rotating annulus using the immersed boundary method
publisher Borntraeger
series Meteorologische Zeitschrift
issn 0941-2948
publishDate 2015-01-01
description We present results of numerical simulations of baroclinic driven flows in the thermally driven rotating annulus using the immersed boundary method for modeling of the boundary conditions. The Navier-Stokes equations in the Boussinesq approximation are solved in the Eulerian flux-form advection scheme with the geophysical flow solver EULAG as numerical framework. We test our approach against results of an appropriate laboratory experiment with water as working fluid and directly aim at the wavy flow regime where complex flows and regular wave patterns are generally observed but where centrifugal effects and turbulence is of minor importance. Multivariate statistical methods are used for analyzing time series of computed temperature data. We, here, present the outcome of the time series data analysis at particular parameter points, and specifically analyze a complex wave-wave interaction, and, secondly, a wave mode switch where the azimuthal wave number changes to the next higher one. The numerical results are highly consistent with the experimental observations. That encourage us to focus on our actual goal as the next step, that is the irregular flow regime found at large rotation rates where the centrifugal force has an increasing effect on flow states and where multiple scale flows are generally observed.
topic baroclinic driven flows
thermally driven rotating annulus
numerical experiments
immersed boundary method
complex flow regimes
multivariate time series analysis
url http://dx.doi.org/10.1127/metz/2014/0609
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