Comparison of Bulk and Bin Warm-Rain Microphysics Models Using a Kinematic Framework

By Hugh Morrison, Wojciech W. Grabowski. 2007

205 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/ed76cf254ab2107cd0f6a47ed5ccb0cd5e5a5003

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Citations in the corpus

A Comparison of TWP-ICE Observational Data with Cloud-Resolving Model Results (2012, methodology): “EULAG-2 uses a 4 of 28 single size distribution for all ice that is further characterized by a prognostic rimed mass fraction [Morrison and Grabowski, 2007, 2008a, 2008b].”
Modeling Supersaturation and Subgrid-Scale Mixing with Two-Moment Bulk Warm Microphysics (2008, methodology): “This work builds upon the framework developed in Morrison et al. (2005) and tested against the detailed microphysics model in Morrison and Grabowski (2007).”
A new two-moment bulk stratiform cloud microphysics scheme in the Community Atmosphere Model, version 3 (CAM3). Part I: Description and numerical tests (2008, background): “2005; Morrison and Grabowski 2007; Phillips et al. 2007).”
Confronting the Challenge of Modeling Cloud and Precipitation Microphysics (2020, unknown): “…schemes for weather and climate models (e.g., Berry & Reinhardt, 1974d; Chen & Liu, 2004; Fan et al., 2012; Feingold et al., 1998; Khairoutdinov & Kogan, 2000; Kogan, 2013; Kogan & Belochitski, 2012; Lebo et al., 2012; Morrison & Grabowski, 2007; Shipway & Hill, 2012; Seifert, 2008; among many).”
A Novel Approach for Representing Ice Microphysics in Models: Description and Tests Using a Kinematic Framework (2007, methodology): “This paper documents the extension of an existing two-moment warm bulk microphysics scheme (Morrison and Grabowski 2006) to the ice phase using this new approach.”
Representation of microphysical processes in cloud‐resolving models: Spectral (bin) microphysics versus bulk parameterization (2015, methodology): “…models with prescribed velocity fields, thereby allowing for the advective and gravitational transport of hydrometeors [Szumowski et al., 1998; Stevens et al., 2005;Morrison and Grabowski, 2007; Ackerman et al., 2009; Fridlind et al., 2012; Shipway and Hill, 2012; Ovchinnikov et al., 2013, 2014].”
The dependence of aerosol effects on clouds and precipitation on cloud‐system organization, shear and stability (2008, methodology): “Hence bulk microphysics schemes remain a viable approach for the simulation of mesoscale systems [Morrison and Grabowski, 2007].”
Parameterization of Cloud Microphysics Based on the Prediction of Bulk Ice Particle Properties. Part I: Scheme Description and Idealized Tests (2015, methodology): “…Process Formulations a. Droplet and crystal nucleation In the version of the schemewith prognosticNc, droplet activation is given by Morrison and Grabowski (2007, 2008b), assuming a constant background aerosol concentration and that the concentration of previously activated cloud condensation…”
On the Parameterization of Evaporation of Raindrops as Simulated by a One-Dimensional Rainshaft Model (2008, background): “Khairoutdinov and Kogan (2000), Milbrandt and Yau (2005b), and Morrison and Grabowski (2007) assume that 1; that is, that the mean volume diameter does not change during evaporation.”