A new two-moment bulk stratiform cloud microphysics scheme in the Community Atmosphere Model, version 3 (CAM3). Part I: Description and numerical tests
By Hugh Morrison, Andrew Gettelman. 2008
1,076 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/a37818a9c5de6eab93b7a9d8cbc2114a455e0e01
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In Atmospheric Science
- Andrew Gettelman
- Hugh Morrison
- Xiaohong Liu
- Steven Ghan
- C. Hoose
- Sungsu Park
- J. Kristjánsson
- R. Easter
In Global and Planetary Change
- Andrew Gettelman
- Hugh Morrison
- Xiaohong Liu
- Steven Ghan
- C. Hoose
- Sungsu Park
- J. Kristjánsson
- R. Easter
Citations in the corpus
- Evidence of liquid dependent ice nucleation in high‐latitude stratiform clouds from surface remote sensors (2011, background): “Many microphysical schemes allow nucleation of ice below water saturation when −25 C ≤ T ≤ 10 C [e.g., Lin et al., 1983; Hong et al., 2004; Morrison and Gettelman, 2008 ].”
- Intercomparison of the cloud water phase among global climate models (2014, background): “3374 stratiform clouds are predicted [Morrison and Gettelman, 2008].”
- The Non-hydrostatic Icosahedral Atmospheric Model: description and development (2014, methodology): “…et al. 2008; Tomita 2008b), and the double-moment bulk method predicts the number concentration in addition to the mass concentration (Meyers et al. 1997; Feingold et al. 1998; Morrison et al. 2005; Seifert and Beheng 2006; Phillips et al. 2007; Morrison and Gettelman 2008; Lim and Hong 2010).”
- The Mean Climate of the Community Atmosphere Model (CAM4) in Forced SST and Fully Coupled Experiments (2013, background): “…a result of the shift in ice cloud closure from a purely relative humidity based formulation in CAM3 and CAM4 (Zhang et al. 2003) to a scheme that allows ice supersaturation (Gettelman et al. 2010) when working in concert with the new CAM5 two-moment micro-physics (Morrison and Gettelman 2008).”
- A Classical-Theory-Based Parameterization of Heterogeneous Ice Nucleation by Mineral Dust, Soot, and Biological Particles in a Global Climate Model (2010, methodology): “Parameterizations that are used in large-scale models are mostly empirical (Lohmann 2002; Lohmann and Diehl 2006; Hoose et al. 2008; Morrison and Gettelman 2008; Phillips et al. 2008; Storelvmo et al. 2008a).”
- An improved representation of the raindrop size distribution for single‐moment microphysics schemes (2012, background): “…is typically represented with either a gamma distribution (Ferrier, 1994; Morrison et al., 2005) or an exponential distribution (Lin et al., 1983; Rutledge and Hobbs, 1983; Fowler et al., 1996; Wilson and Ballard, 1999; Seifert and Beheng, 2006; Morrison and Gettelman, 2008; Thompson et al., 2008).”
- Seamless Stratocumulus Simulation across the Turbulent Gray Zone (2014, methodology): “…parameterizations of the subgrid variability of cloud and rainwater at different spatial scales, and presented a method of using these parameterizations to correct microphysical process rates for this bias, following methods similar to Morrison and Gettelman (2008) and Larson and Griffin (2013).”
- The Evolution of Climate Sensitivity and Climate Feedbacks in the Community Atmosphere Model (2012, background): “The new two-moment stratiform cloud micro-physics scheme (Gettelman et al. 2010; Morrison and Gettelman 2008) includes aerosol activation of cloud drops/crystals for liquid and ice, explicitly treating aerosol–cloud interactions.”
- Aerosol indirect effects – general circulation model intercomparison and evaluation with satellite data (2009, neutral): “The modifi-cations include new two-moment microphysics (Gettelman et al., 2008; Morrison and Gettelman, 2008) including a physically based method for the aerosol activation of cloud droplets (Abdul-Razzak and Ghan, 2000), a diagnostic cloud cover scheme based on relative humidity after Slingo (1987)…”
- Enhanced Solar Energy Absorption by Internally-Mixed Black Carbon in Snow Grains (2012, background): “…MAM7-CAM5, aerosols interact with clouds through activation, transport, aqueous chemistry, and resuspension, thereby influencing the aerosol amounts that exist interstitially and within cloud hydrometeors (Easter et al., 2004; Ghan and Easter, 2006; Morrison and Gettelman, 2008; Liu et al., 2012).”
- Understanding Cloud and Convective Characteristics in Version 1 of the E3SM Atmosphere Model (2018, methodology): “Version 2 of Morrison and Gettelman (2008) represents an update to the MG2008 microphysics scheme used in CAM5.”