DOE PAGES title logo U.S. Department of Energy
Office of Scientific and Technical Information

Title: Exploring a Lower‐Resolution Physics Grid in CAM‐SE‐CSLAM

Abstract

This paper describes the implementation of a coarser-resolution physics grid into the Community Atmosphere Model (CAM), containing $$5\over{9}$$ fewer grid columns than the dynamics grid. The dry dynamics is represented by the spectral element dynamical core, and tracer transport is computed using the Conservative Semi-Lagrangian Finite Volume Method (CAM-SE-CSLAM). Algorithms are presented that map fields between the dynamics and physics grids while maintaining numerical properties ideal for atmospheric simulations such as mass conservation and mixing ratio shape and linear-correlation preservation. The results of experiments using the lower-resolution physics grid are compared to the conventional method in which the physics and dynamical grids coincide. The lower-resolution physics grid provides a volume mean state to the physics computed from an equal sampling of the different types of nodal solutions arising in the spectral-element method and effectively mitigates grid imprinting in regions with steep topography. The impact of the coarser-resolution physics grid on the resolved scales of motion is analyzed in an aqua planet configuration, across a range of dynamical core grid resolutions. The results suggest that the effective resolution of the model is not degraded through the use of a coarser-resolution physics grid. Since the physics makes up about half the computational cost of the conventional CAM-SE-CSLAM configuration, the coarser physics grid may allow for significant cost savings with little to no downside

Authors:
ORCiD logo [1]; ORCiD logo [2]; ORCiD logo [1];  [2]; ORCiD logo [2]
  1. School of Marine and Atmospheric SciencesStony Brook University Stony Brook NY USA
  2. National Center for Atmospheric Research Boulder CO USA
Publication Date:
Research Org.:
Univ. of Georgia, Athens, GA (United States)
Sponsoring Org.:
USDOE Office of Science (SC)
OSTI Identifier:
1560186
Alternate Identifier(s):
OSTI ID: 1560188; OSTI ID: 1613245
Grant/Contract Number:  
SC0019459; 12-015334
Resource Type:
Published Article
Journal Name:
Journal of Advances in Modeling Earth Systems
Additional Journal Information:
Journal Name: Journal of Advances in Modeling Earth Systems Journal Volume: 11 Journal Issue: 7; Journal ID: ISSN 1942-2466
Publisher:
American Geophysical Union (AGU)
Country of Publication:
United States
Language:
English
Subject:
37 INORGANIC, ORGANIC, PHYSICAL, AND ANALYTICAL CHEMISTRY; 54 ENVIRONMENTAL SCIENCES; Meteorology & Atmospheric Sciences

Citation Formats

Herrington, Adam R., Lauritzen, Peter H., Reed, Kevin A., Goldhaber, Steve, and Eaton, Brian E. Exploring a Lower‐Resolution Physics Grid in CAM‐SE‐CSLAM. United States: N. p., 2019. Web. doi:10.1029/2019MS001684.
Herrington, Adam R., Lauritzen, Peter H., Reed, Kevin A., Goldhaber, Steve, & Eaton, Brian E. Exploring a Lower‐Resolution Physics Grid in CAM‐SE‐CSLAM. United States. https://doi.org/10.1029/2019MS001684
Herrington, Adam R., Lauritzen, Peter H., Reed, Kevin A., Goldhaber, Steve, and Eaton, Brian E. Wed . "Exploring a Lower‐Resolution Physics Grid in CAM‐SE‐CSLAM". United States. https://doi.org/10.1029/2019MS001684.
@article{osti_1560186,
title = {Exploring a Lower‐Resolution Physics Grid in CAM‐SE‐CSLAM},
author = {Herrington, Adam R. and Lauritzen, Peter H. and Reed, Kevin A. and Goldhaber, Steve and Eaton, Brian E.},
abstractNote = {This paper describes the implementation of a coarser-resolution physics grid into the Community Atmosphere Model (CAM), containing $5\over{9}$ fewer grid columns than the dynamics grid. The dry dynamics is represented by the spectral element dynamical core, and tracer transport is computed using the Conservative Semi-Lagrangian Finite Volume Method (CAM-SE-CSLAM). Algorithms are presented that map fields between the dynamics and physics grids while maintaining numerical properties ideal for atmospheric simulations such as mass conservation and mixing ratio shape and linear-correlation preservation. The results of experiments using the lower-resolution physics grid are compared to the conventional method in which the physics and dynamical grids coincide. The lower-resolution physics grid provides a volume mean state to the physics computed from an equal sampling of the different types of nodal solutions arising in the spectral-element method and effectively mitigates grid imprinting in regions with steep topography. The impact of the coarser-resolution physics grid on the resolved scales of motion is analyzed in an aqua planet configuration, across a range of dynamical core grid resolutions. The results suggest that the effective resolution of the model is not degraded through the use of a coarser-resolution physics grid. Since the physics makes up about half the computational cost of the conventional CAM-SE-CSLAM configuration, the coarser physics grid may allow for significant cost savings with little to no downside},
doi = {10.1029/2019MS001684},
journal = {Journal of Advances in Modeling Earth Systems},
number = 7,
volume = 11,
place = {United States},
year = {Wed Jul 10 00:00:00 EDT 2019},
month = {Wed Jul 10 00:00:00 EDT 2019}
}

Journal Article:
Free Publicly Available Full Text
Publisher's Version of Record
https://doi.org/10.1029/2019MS001684

Citation Metrics:
Cited by: 12 works
Citation information provided by
Web of Science

Save / Share:

Works referenced in this record:

Petascale atmospheric models for the Community Climate System Model: new developments and evaluation of scalable dynamical cores
journal, July 2008


A Proposal for the Intercomparison of the Dynamical Cores of Atmospheric General Circulation Models
journal, October 1994


Believable Scales and Parameterizations in a Spectral Transform Model
journal, February 1997


Vertical Velocity in the Gray Zone: VERTICAL VELOCITY IN THE GRAY ZONE
journal, October 2017

  • Jeevanjee, Nadir
  • Journal of Advances in Modeling Earth Systems, Vol. 9, Issue 6
  • DOI: 10.1002/2017MS001059

A Total Energy Error Analysis of Dynamical Cores and Physics‐Dynamics Coupling in the Community Atmosphere Model (CAM)
journal, May 2019

  • Lauritzen, Peter H.; Williamson, David L.
  • Journal of Advances in Modeling Earth Systems, Vol. 11, Issue 5
  • DOI: 10.1029/2018MS001549

An Idealized Test of the Response of the Community Atmosphere Model to Near‐Grid‐Scale Forcing Across Hydrostatic Resolutions
journal, February 2018

  • Herrington, A. R.; Reed, K. A.
  • Journal of Advances in Modeling Earth Systems, Vol. 10, Issue 2
  • DOI: 10.1002/2017MS001078

CAM-SE–CSLAM: Consistent Coupling of a Conservative Semi-Lagrangian Finite-Volume Method with Spectral Element Dynamics
journal, March 2017

  • Lauritzen, Peter Hjort; Taylor, Mark A.; Overfelt, James
  • Monthly Weather Review, Vol. 145, Issue 3
  • DOI: 10.1175/MWR-D-16-0258.1

Breaking the Cloud Parameterization Deadlock
journal, November 2003

  • Randall, David; Khairoutdinov, Marat; Arakawa, Akio
  • Bulletin of the American Meteorological Society, Vol. 84, Issue 11
  • DOI: 10.1175/BAMS-84-11-1547

Short‐term time step convergence in a climate model
journal, February 2015

  • Wan, Hui; Rasch, Philip J.; Taylor, Mark A.
  • Journal of Advances in Modeling Earth Systems, Vol. 7, Issue 1
  • DOI: 10.1002/2014MS000368

A standard test case suite for two-dimensional linear transport on the sphere
journal, January 2012

  • Lauritzen, P. H.; Skamarock, W. C.; Prather, M. J.
  • Geoscientific Model Development, Vol. 5, Issue 3
  • DOI: 10.5194/gmd-5-887-2012

CAM-SE: A scalable spectral element dynamical core for the Community Atmosphere Model
journal, November 2011

  • Dennis, John M.; Edwards, Jim; Evans, Katherine J.
  • The International Journal of High Performance Computing Applications, Vol. 26, Issue 1
  • DOI: 10.1177/1094342011428142

Computational aspects of a scalable high-order discontinuous Galerkin atmospheric dynamical core
journal, February 2009


NCAR Release of CAM‐SE in CESM2.0: A Reformulation of the Spectral Element Dynamical Core in Dry‐Mass Vertical Coordinates With Comprehensive Treatment of Condensates and Energy
journal, July 2018

  • Lauritzen, P. H.; Nair, R. D.; Herrington, A. R.
  • Journal of Advances in Modeling Earth Systems, Vol. 10, Issue 7
  • DOI: 10.1029/2017MS001257

A class of deformational flow test cases for linear transport problems on the sphere
journal, November 2010

  • Nair, Ramachandran D.; Lauritzen, Peter H.
  • Journal of Computational Physics, Vol. 229, Issue 23
  • DOI: 10.1016/j.jcp.2010.08.014

The design and application of upwind schemes on unstructured meshes
conference, February 2013

  • Barth, Timothy; Jespersen, Dennis
  • 27th Aerospace Sciences Meeting
  • DOI: 10.2514/6.1989-366

An Explanation for the Sensitivity of the Mean State of the Community Atmosphere Model to Horizontal Resolution on Aquaplanets
journal, July 2017


Comparison of dynamical cores for NWP models: comparison of COSMO and Dune
journal, April 2012

  • Brdar, Slavko; Baldauf, Michael; Dedner, Andreas
  • Theoretical and Computational Fluid Dynamics, Vol. 27, Issue 3-4
  • DOI: 10.1007/s00162-012-0264-z

On a fundamental problem in implementing flux-form advection schemes for tracer transport in 3-dimensional general circulation and chemistry transport models
journal, April 2001

  • Jöckel, P.; von Kuhlmann, R.; Lawrence, M. G.
  • Quarterly Journal of the Royal Meteorological Society, Vol. 127, Issue 573
  • DOI: 10.1002/qj.49712757318

A kinetic energy backscatter algorithm for use in ensemble prediction systems
journal, October 2005

  • Shutts, Glenn
  • Quarterly Journal of the Royal Meteorological Society, Vol. 131, Issue 612
  • DOI: 10.1256/qj.04.106

Reference aquaplanet climate in the C ommunity A tmosphere M odel, V ersion 5
journal, January 2016

  • Medeiros, Brian; Williamson, David L.; Olson, Jerry G.
  • Journal of Advances in Modeling Earth Systems, Vol. 8, Issue 1
  • DOI: 10.1002/2015MS000593

The Resolution Dependence of Explicitly Modeled Convective Systems
journal, April 1997


Dependence of aqua-planet simulations on time step
journal, April 2003

  • Williamson, David L.; Olson, Jerry G.
  • Quarterly Journal of the Royal Meteorological Society, Vol. 129, Issue 591
  • DOI: 10.1256/qj.02.62

First- and Second-Order Conservative Remapping Schemes for Grids in Spherical Coordinates
journal, September 1999


The effect of time steps and time-scales on parametrization suites
journal, August 2012

  • Williamson, David L.
  • Quarterly Journal of the Royal Meteorological Society, Vol. 139, Issue 671
  • DOI: 10.1002/qj.1992

Effective buoyancy at the surface and aloft: Effective Buoyancy
journal, November 2015

  • Jeevanjee, Nadir; Romps, David M.
  • Quarterly Journal of the Royal Meteorological Society, Vol. 142, Issue 695
  • DOI: 10.1002/qj.2683

Sensitivity of Radiative–Convective Equilibrium Simulations to Horizontal Resolution
journal, July 2006

  • Pauluis, Olivier; Garner, Stephen
  • Journal of the Atmospheric Sciences, Vol. 63, Issue 7
  • DOI: 10.1175/JAS3705.1

A conservative semi-Lagrangian multi-tracer transport scheme (CSLAM) on the cubed-sphere grid
journal, March 2010

  • Lauritzen, Peter H.; Nair, Ramachandran D.; Ullrich, Paul A.
  • Journal of Computational Physics, Vol. 229, Issue 5
  • DOI: 10.1016/j.jcp.2009.10.036

Evaluating advection/transport schemes using interrelated tracers, scatter plots and numerical mixing diagnostics
journal, November 2011

  • Lauritzen, P. H.; Thuburn, J.
  • Quarterly Journal of the Royal Meteorological Society, Vol. 138, Issue 665
  • DOI: 10.1002/qj.986

The terminator "toy" chemistry test: a simple tool to assess errors in transport schemes
journal, January 2015

  • Lauritzen, P. H.; Conley, A. J.; Lamarque, J. -F.
  • Geoscientific Model Development, Vol. 8, Issue 5
  • DOI: 10.5194/gmd-8-1299-2015

NCAR global model topography generation software for unstructured grids
journal, January 2015

  • Lauritzen, P. H.; Bacmeister, J. T.; Callaghan, P. F.
  • Geoscientific Model Development Discussions, Vol. 8, Issue 6
  • DOI: 10.5194/gmdd-8-4623-2015

A “Vertically Lagrangian” Finite-Volume Dynamical Core for Global Models
journal, October 2004