Search engine for discovering works of Art, research articles, and books related to Art and Culture
ShareThis
Javascript must be enabled to continue!

Finite-volume discretization of the quasi-geostrophic equations with implicit dissipation

View through CrossRef
We present in this work a new discretization of the multi-layer quasi-geostrophic (QG) model that relies on implicit dissipation rather than additional explicit dissipation.It is first based on the staggered discretization of the potential vorticity (PV) and the stream-function in order to solve the PV advection with a finite volume method.This ensures the exact material conservation of the PV.We compute PV fluxes with a WENO-5 interpolation whose implicit dissipation replaces the usual explicit (hyper-)viscous dissipation.We propose a new method for solving reversibly the elliptic equation which is nontrivial with this staggered discretization.The presented discretization does not require the tuning of any additional parameter, \textit{e.g.} additional hyper-viscosity.We test the proposed method on a challenging idealized wind-driven double-gyre configuration at eddy-resolving, eddy-permitting, and non-eddy-resolving resolutions.In the eddy-permitting and non-eddy-resolving resolutions, our method produces an eastward jet contrary to usual discretizations without parametrization.Moreover, our method produces statistics that have a stronger coherence across resolutions than usual discretizations.We release a very short, concise, and efficient PyTorch implementation of our method to facilitate future data assimilation or machine-learning developments upon this new discretization.
Title: Finite-volume discretization of the quasi-geostrophic equations with implicit dissipation
Description:
We present in this work a new discretization of the multi-layer quasi-geostrophic (QG) model that relies on implicit dissipation rather than additional explicit dissipation.
It is first based on the staggered discretization of the potential vorticity (PV) and the stream-function in order to solve the PV advection with a finite volume method.
This ensures the exact material conservation of the PV.
We compute PV fluxes with a WENO-5 interpolation whose implicit dissipation replaces the usual explicit (hyper-)viscous dissipation.
We propose a new method for solving reversibly the elliptic equation which is nontrivial with this staggered discretization.
The presented discretization does not require the tuning of any additional parameter, \textit{e.
g.
} additional hyper-viscosity.
We test the proposed method on a challenging idealized wind-driven double-gyre configuration at eddy-resolving, eddy-permitting, and non-eddy-resolving resolutions.
In the eddy-permitting and non-eddy-resolving resolutions, our method produces an eastward jet contrary to usual discretizations without parametrization.
Moreover, our method produces statistics that have a stronger coherence across resolutions than usual discretizations.
We release a very short, concise, and efficient PyTorch implementation of our method to facilitate future data assimilation or machine-learning developments upon this new discretization.

Related Results

ISFAA : Implicit SPH for astrophysical apllications
ISFAA : Implicit SPH for astrophysical apllications
Computational simulation is one of the basic techniques of modern Astrophysics. The long-term time astrophysical processes cannot be treated with explicit approaches because that t...
Towards long-term simulations of planetary-scale vortices and storms on Jupiter and Saturn
Towards long-term simulations of planetary-scale vortices and storms on Jupiter and Saturn
Long-term simulations of planetary vortices and storms are essential for improving our understanding of the atmospheric dynamics on gas giants such as Jupiter and Saturn. These sim...
MQGeometry-1.0: a multi-layer quasi-geostrophic solver on non-rectangular geometries
MQGeometry-1.0: a multi-layer quasi-geostrophic solver on non-rectangular geometries
Abstract. This paper presents MQGeometry, a multi-layer quasi-geostrophic (QG) equations solver for non-rectangul ar geometries. We advect the potential voriticity (PV) with finite...
Generated Fuzzy Quasi-ideals in Ternary Semigroups
Generated Fuzzy Quasi-ideals in Ternary Semigroups
Here in this paper, we provide characterizations of fuzzy quasi-ideal in terms of level and strong level subsets. Along with it, we provide expression for the generated fuzzy quasi...
Transition Probabilities of Wind-driven Ocean Flows
Transition Probabilities of Wind-driven Ocean Flows
<div> <div> <div> <p>The quasi-geostrophic wind-driven double-gyre ocean circulation in a midlatitude rectangular basin is a...
Where you aim - not how you aim - affects implicit recalibration in visuomotor adaptation
Where you aim - not how you aim - affects implicit recalibration in visuomotor adaptation
Abstract: The influence of explicit strategies on implicit recalibration during visuomotor adaptation has become a central question in motor learning. Because the two systems opera...
Half-thickness discretized format for simulating compressible delay interbed
Half-thickness discretized format for simulating compressible delay interbed
Abstract The simulation of compressible delay interbed is an important component of ground subsidence modeling. Currently, the most widely used groundwater simulation sof...

Back to Top