A “Vertically Lagrangian” Finite-Volume Dynamical Core for Global Models

By Shian‐Jiann Lin. 2004

1,093 citations recorded by the source corpus.

Subfields: Applied Mathematics, Computational Mechanics

View Paper: https://www.semanticscholar.org/paper/f8f839b21fc442c23fc16eb459ebeadf0929133f

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In Applied Mathematics

In Computational Mechanics

Citations in the corpus

CAS FGOALS-f3-L Model Datasets for CMIP6 Historical Atmospheric Model Intercomparison Project Simulation (2019, methodology): “The atmospheric component, FAMIL, uses a finitevolume dynamical core (Lin, 2004) on a cubed-sphere grid (Putman and Lin, 2007), with six tiles across the globe.”
Warm Pool and Cold Tongue El Nino Events as Simulated by the GFDL 2.1 Coupled GCM (2010, background): “The dynamic core is based on a finite volume (Lin 2004).”
Toward Convective-Scale Prediction within the Next Generation Global Prediction System (2019, methodology): “The FV3 in fvGFS uses the “vertically Lagrangian” dynamics of Lin (2004) extended with the nonhydrostatic pressure gradient computation of Lin (1997) and a semi-implicit solver for vertically propagating sound waves, discretized on the cubedsphere grid of Putman and Lin (2007).”
The MERRA-2 Aerosol Reanalysis, 1980 - onward, Part I: System Description and Data Assimilation Evaluation. (2017, methodology): “The discretization of the dynamical core (Lin 2004) is computed on a cubed sphere grid that mitigates grid-spacing singularities (Putman and Lin 2007).”
Volcanic signals in oceans (2009, methodology): “The dynamical core is based on the finite volume scheme of Lin [2004] .”
The pros and cons of diffusion, filters and fixers in Atmospheric General Circulation Models (2011, methodology): “The rotational motions are damped via inherent numerical diffusion as shown later (see also Lin (2004)).”
GFDL's CM2 Global Coupled Climate Models. Part I: Formulation and Simulation Characteristics (2006, background): “Part III: Tropical Pacific climate and ENSO.”
Adjoint sensitivity of the model forecast to data assimilation system error covariance parameters (2010, methodology): “GEOS5 DAS consists of the GEOS-5 general circulation model comprising: finite-volume dynamics (Lin, 2004) and Goddard-developed physics; the adjoint of the finite-volume dynamics (Giering et al., 2005) which accounts for simple vertical diffusion; the Grid-point Statistical Interpolation (GSI)…”
Finite-volume transport on various cubed-sphere grids (2007, methodology): “The finite-volume dynamical core (FV core hereafter; [1]) has been generalized for quasi-uniform cubedsphere grids in general non-orthogonal curvilinear coordinates using the National Oceanic and Atmospheric Administration (NOAA) Geophysical Fluid Dynamics Laboratory’s (GFDL) Flexible Modeling Syste”
The Mean Climate of the Community Atmosphere Model (CAM4) in Forced SST and Fully Coupled Experiments (2013, methodology): “The FV dynamical core, available as an option in CAM3 (Lin and Rood 1996; Lin 2004), is now the default option in CAM4.”
The Non-hydrostatic Icosahedral Atmospheric Model: description and development (2014, background): “As for other types of grid models, cubic grids are also candidates for high-resolution atmospheric models (McGregor 1996; Lin 2004; Putman and Suarez 2011).”
The Low-Resolution CCSM4 (2012, methodology): “The intermediate-resolution CCSM4 utilizes the ﬁnite-volume (FV) dynamical core (Lin 2004) with a nominal 2 8 atmosphere and land horizontal grid (1.9 8 3 2.5 8 latitude versus longitude) with 26 atmospheric layers in the vertical and a nominal 1 8 ocean and ice horizontal grid (referred to as x1)…”
Goddard Earth Observing System chemistry‐climate model simulations of stratospheric ozone‐temperature coupling between 1950 and 2005 (2008, methodology): “This dynamical core [ Lin, 2004 ] retains the conservation properties of the transport code and uses a novel quasi-Lagrangian vertical coordinate [Lin and Rood, 1997] that allows for accurate computation of vertical motions.”
Toward a Minimal Representation of Aerosols in Climate Models: Comparative Decomposition of Aerosol Direct, Semidirect, and Indirect Radiative Forcing (2012, methodology): “…treatment of turbulence in CAM.1 is described by Bretherton and Park (2009), and its performance is evaluated by Park and Bretherton (2009). e. Resolved transport Transport of water and other trace species is calculated by the Lin–Rood finite-volume core (Lin and Rood 1996; Lin 2004).”