Description of the NCAR Community Atmosphere Model (CAM 3.0)
By Richard B. Neale, J. Richter, Andrew J. Conley, Sungsu Park, Peter H. Lauritzen, Andrew Gettelman, David L. Williamson. 2004
2,589 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/7d46f5d8524d695073eb464f12695387ee74f57c
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Atmospheric Science
- Hugh Morrison
- Andrew Gettelman
- Chris Bretherton
- J. Golaz
- Peter M. Caldwell
- P. Bogenschutz
- Stephen A. Klein
- V. Larson
In Global and Planetary Change
- Hugh Morrison
- Andrew Gettelman
- Chris Bretherton
- J. Golaz
- Peter M. Caldwell
- Stephen A. Klein
- P. Bogenschutz
- V. Larson
Citations in the corpus
- The Role of Convective Moistening in the Madden–Julian Oscillation (2009, methodology): “Within each grid column, all cloud tops and cloud updraft detrainment are forced to be above the midtropospheric minimum of saturation moist static energy (Collins et al. 2004).”
- STABILIZING CLOUD FEEDBACK DRAMATICALLY EXPANDS THE HABITABLE ZONE OF TIDALLY LOCKED PLANETS (2013, methodology): “E P] 1 J ul 2”
- On the computation of planetary boundary-layer height using the bulk Richardson number method (2014, methodology): “11), which is close to that used in CAM4 (Ribc = 0.3; Neale et al., 2010).”
- Aerosol–climate interactions in the Norwegian Earth System Model – NorESM1-M (2012, methodology): “cldtunorig As Ctrl, but tuning of cloud microphysics as in NCAR CAM4 (Neale et al., 2010).”
- Global Mean Climate and Main Patterns of Variability in the CMCC‐CM2 Coupled Model (2018, methodology): “For these configurations version 4 of the CAMmodel (CAM4; Neale et al., 2010) is used with a prescribed aerosols physics.”
- Prognostic Validation of a Neural Network Unified Physics Parameterization (2018, result): “We compare the performance of our NN scheme to the single-column version of the CAM version 5 (Neale et al., 2012).”
- Understanding Cloud and Convective Characteristics in Version 1 of the E3SM Atmosphere Model (2018, methodology): “3 (CAM5.3; Neale et al., 2012), which has a resolution of 1° in horizontal and 30 layers in vertical, but it adopts the SE dynamical core (Dennis et al.”
- A baroclinic instability test case for atmospheric model dynamical cores (2006, methodology): “In contrast, alternative schemes, like a spectral transform Eulerian method (Collins et al. 2004) or a finite-difference approach on an icosahedral grid (Majewski et al. 2002), generally apply a rather scale-selective fourth-order horizontal diffusion mechanism to prevent the accumulation of…”