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Aquaplanet Experiments Using CAM’s Variable-Resolution Dynamical Core
by
Ullrich, Paul A.
, Zarzycki, Colin M.
, Levy, Michael N.
, Taylor, Mark A.
, Overfelt, James R.
, Jablonowski, Christiane
in
Aerosols
/ Atmospheric models
/ Boundary conditions
/ Climate
/ Climate models
/ Climatology
/ Climatology. Bioclimatology. Climate change
/ Clouds
/ Cyclones
/ Earth, ocean, space
/ Equator
/ Equatorial regions
/ Exact sciences and technology
/ External geophysics
/ Finite element method
/ General circulation models
/ Geophysics. Techniques, methods, instrumentation and models
/ Grid refinement (mathematics)
/ Imprinting
/ Laboratories
/ Meteorology
/ Modeling
/ Parameterization
/ Performance evaluation
/ Physics
/ Precipitation
/ Quadrilaterals
/ Regions
/ Resolution
/ Scaling
/ Simulation
/ Simulations
/ Statistical methods
/ Studies
/ Wave propagation
2014
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Aquaplanet Experiments Using CAM’s Variable-Resolution Dynamical Core
by
Ullrich, Paul A.
, Zarzycki, Colin M.
, Levy, Michael N.
, Taylor, Mark A.
, Overfelt, James R.
, Jablonowski, Christiane
in
Aerosols
/ Atmospheric models
/ Boundary conditions
/ Climate
/ Climate models
/ Climatology
/ Climatology. Bioclimatology. Climate change
/ Clouds
/ Cyclones
/ Earth, ocean, space
/ Equator
/ Equatorial regions
/ Exact sciences and technology
/ External geophysics
/ Finite element method
/ General circulation models
/ Geophysics. Techniques, methods, instrumentation and models
/ Grid refinement (mathematics)
/ Imprinting
/ Laboratories
/ Meteorology
/ Modeling
/ Parameterization
/ Performance evaluation
/ Physics
/ Precipitation
/ Quadrilaterals
/ Regions
/ Resolution
/ Scaling
/ Simulation
/ Simulations
/ Statistical methods
/ Studies
/ Wave propagation
2014
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Aquaplanet Experiments Using CAM’s Variable-Resolution Dynamical Core
by
Ullrich, Paul A.
, Zarzycki, Colin M.
, Levy, Michael N.
, Taylor, Mark A.
, Overfelt, James R.
, Jablonowski, Christiane
in
Aerosols
/ Atmospheric models
/ Boundary conditions
/ Climate
/ Climate models
/ Climatology
/ Climatology. Bioclimatology. Climate change
/ Clouds
/ Cyclones
/ Earth, ocean, space
/ Equator
/ Equatorial regions
/ Exact sciences and technology
/ External geophysics
/ Finite element method
/ General circulation models
/ Geophysics. Techniques, methods, instrumentation and models
/ Grid refinement (mathematics)
/ Imprinting
/ Laboratories
/ Meteorology
/ Modeling
/ Parameterization
/ Performance evaluation
/ Physics
/ Precipitation
/ Quadrilaterals
/ Regions
/ Resolution
/ Scaling
/ Simulation
/ Simulations
/ Statistical methods
/ Studies
/ Wave propagation
2014
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Aquaplanet Experiments Using CAM’s Variable-Resolution Dynamical Core
Journal Article
Aquaplanet Experiments Using CAM’s Variable-Resolution Dynamical Core
2014
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Overview
A variable-resolution option has been added within the spectral element (SE) dynamical core of the U.S. Department of Energy (DOE)–NCAR Community Atmosphere Model (CAM). CAM-SE allows for static refinement via conforming quadrilateral meshes on the cubed sphere. This paper investigates the effect of mesh refinement in a climate model by running variable-resolution (var-res) simulations on an aquaplanet. The variable-resolution grid is a 2° (∼222 km) grid with a refined patch of 0.25° (∼28 km) resolution centered at the equator. Climatology statistics from these simulations are compared to globally uniform runs of 2° and 0.25°.
A significant resolution dependence exists when using the CAM version 4 (CAM4) subgrid physical parameterization package across scales. Global cloud fraction decreases and equatorial precipitation increases with finer horizontal resolution, resulting in drastically different climates between the uniform grid runs and a physics-induced grid imprinting in the var-res simulation. Using CAM version 5 (CAM5) physics significantly improves cloud scaling at different grid resolutions. Additional precipitation at the equator in the high-resolution mesh results in collocated zonally anomalous divergence in both var-res simulations, although this feature is much weaker in CAM5 than CAM4. The equilibrium solution at each grid spacing within the var-res simulations captures the majority of the resolution signal of the corresponding globally uniform grids. The var-res simulation exhibits good performance with respect to wave propagation, including equatorial regions where waves pass through grid transitions. In addition, the increased frequency of high-precipitation events in the refined 0.25° area within the var-res simulations matches that observed in the global 0.25° simulations.
Publisher
American Meteorological Society
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