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

MQGeometry-1.0: a multi-layer quasi-geostrophic solver on non-rectangular geometries

View through CrossRef
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 volumes to ensure global PV conservation thanks to a staggered discretization of the PV and stream-function (SF). Thanks to this staggering, the PV is defined inside the domain, removing the need for defining the PV on the domain's boundary. We compute PV fluxes with upwind-biased interpolations whose implicit dissipation replaces the usual explicit (hyper-)viscous dissipation. The presented discretization does not require the tuning of any additional parameter, e.g. additional eddy viscosity. We solve the QG elliptic equation with a fast discrete sine transform spectral solver on rectangular geometry. We extend this fast solver to non-rectangular geometries using the capacitance matrix method. We validate our solver on a vortex-shear instability test case in a circular domain, a vortex-wall interaction test-case, and on an idealized wind-driven double-gyre configuration in a octogonal domain at a eddy-permitting resolution. We release a concise, efficient, and auto-differentiable PyTorch implementation of our method to facilitate future developments upon this new discretization, e.g. machine learning parameterization or data-assimilation techniques.
Title: MQGeometry-1.0: a multi-layer quasi-geostrophic solver on non-rectangular geometries
Description:
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 volumes to ensure global PV conservation thanks to a staggered discretization of the PV and stream-function (SF).
Thanks to this staggering, the PV is defined inside the domain, removing the need for defining the PV on the domain's boundary.
We compute PV fluxes with upwind-biased interpolations whose implicit dissipation replaces the usual explicit (hyper-)viscous dissipation.
The presented discretization does not require the tuning of any additional parameter, e.
g.
additional eddy viscosity.
We solve the QG elliptic equation with a fast discrete sine transform spectral solver on rectangular geometry.
We extend this fast solver to non-rectangular geometries using the capacitance matrix method.
We validate our solver on a vortex-shear instability test case in a circular domain, a vortex-wall interaction test-case, and on an idealized wind-driven double-gyre configuration in a octogonal domain at a eddy-permitting resolution.
We release a concise, efficient, and auto-differentiable PyTorch implementation of our method to facilitate future developments upon this new discretization, e.
g.
machine learning parameterization or data-assimilation techniques.

Related Results

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...
Advanced routing mechanisms in ASON/GMPLS networks
Advanced routing mechanisms in ASON/GMPLS networks
Current network infrastructures are supported on a layered model whereby heterogeneous data traffic can be seamlessly transported. In this architecture, where client/server relatio...
Synchronizability and eigenvalues of two-layer star networks
Synchronizability and eigenvalues of two-layer star networks
From the study of multilayer networks, scientists have found that the properties of the multilayer networks show great difference from those of the traditional complex networks. In...
Penetrative convection in Nocturnal ABL: Numerical Simulations
Penetrative convection in Nocturnal ABL: Numerical Simulations
<p>After the sunset, under calm and clear sky conditions, aerosol laden surface air-layer, cools rapidly due to radiative cooling<sup>[1, 2, & 3...
A holistic aerosol model for Uranus and Neptune, including Dark Spots
A holistic aerosol model for Uranus and Neptune, including Dark Spots
<p>Previous studies of the reflectance spectra of Uranus and Neptune concentrated on individual, narrow wavelength regions, inferring solutions for the vertical struc...

Back to Top