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Todd D. Ringler

Researcher at Los Alamos National Laboratory

Publications -  73
Citations -  4216

Todd D. Ringler is an academic researcher from Los Alamos National Laboratory. The author has contributed to research in topics: Potential vorticity & Shallow water equations. The author has an hindex of 34, co-authored 72 publications receiving 3374 citations. Previous affiliations of Todd D. Ringler include Cornell University & Colorado State University.

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The DOE E3SM Coupled Model Version 1: Overview and Evaluation at Standard Resolution

Jean-Christophe Golaz, +86 more
TL;DR: Energy Exascale Earth System Model (E3SM) project as mentioned in this paper is a project of the U.S. Department of Energy that aims to develop and validate the E3SM model.
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A Multiscale Nonhydrostatic Atmospheric Model Using Centroidal Voronoi Tesselations and C-Grid Staggering

TL;DR: The formulation of a fully compressible nonhydrostatic atmospheric model called the Model for Prediction Across Scales–Atmosphere (MPAS-A) is described, using centroidal Voronoi meshes and a C-grid staggering of the prognostic variables to incorporate a split-explicit time-integration technique used in many existing meso- and cloud-scale models.
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A multi-resolution approach to global ocean modeling

TL;DR: In this paper, a new global ocean model (MPASO-Ocean) capable of using enhanced resolution in selected regions of the ocean domain is described and evaluated, and three simulations using different grids are presented.
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A unified approach to energy conservation and potential vorticity dynamics for arbitrarily-structured C-grids

TL;DR: A numerical scheme applicable to arbitrarily-structured C-grids is presented for the nonlinear shallow-water equations, using the vector-invariant form of the momentum equation to guarantee that mass, velocity and potential vorticity evolve in a consistent and compatible manner.
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Numerical representation of geostrophic modes on arbitrarily structured C-grids

TL;DR: An explicit formula is given for constructing an appropriate discretization of the Coriolis terms and it is confirmed that the scheme does indeed give stationary geostrophic modes for the hexagonal-pentagonal and triangular geodesic C-grids on the sphere.