Freezing Drizzle Formation in Stably Stratified Layer Clouds: The Role of Radiative Cooling of Cloud Droplets, Cloud Condensation Nuclei, and Ice Initiation

By R. Rasmussen, I. Geresdi, Gregory Thompson, Kevin W. Manning, Elizabeth F. Karplus. 2002

146 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/8db011ebe2755b6d27fbbc6a72f5374a7d00dff1

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Citations in the corpus

A Novel Approach for Representing Ice Microphysics in Models: Description and Tests Using a Kinematic Framework (2007, methodology): “A similar separation of unrimed crystals, graupel, and/or hail is employed by many bin microphysics models (e.g., Geresdi 1998; Ovtchinnikov and Kogan 2000; Rasmussen et al. 2002).”
A New Visibility Parameterization for Warm-Fog Applications in Numerical Weather Prediction Models (2006, methodology): “Although droplet number concentration can be a prognostic variable in mesoscale models (Rasmussen et al. 2002), the bulk microphysical parameterizations, usually with one or two variables for each hydrometeor category, use predescribed size distributions.”
Parameterization of the Autoconversion Process. Part I: Analytical Formulation of the Kessler-Type Parameterizations (2004, background): “…is important for understanding the interactions between cloud microphysics and cloud dynamics (e.g., Chen and Cotton 1987), for the forecasting of the freezing drizzle formation and aircraft icing (Rasmussen et al. 2002), and for improving the treatment of clouds in climate models (Rotstayn 2000).”
Microbiology and atmospheric processes: the role of biological particles in cloud physics (2007, unknown): “This evidence comes from observing the onset of ice formation in clouds with simple motions and cloud regions where the action of primary ice nucleation processes is expected to be isolated (e.g., Cooper and Vali, 1981; Cooper, 1986; Rasmussen et al., 2002).”
Explicit Forecasts of Winter Precipitation Using an Improved Bulk Microphysics Scheme. Part I: Description and Sensitivity Analysis (2004, methodology): “Improvements to the bulk scheme were made in order to reproduce results of the bin microphysics model of Rasmussen et al. (2002).”
Spectral (Bin) microphysics coupled with a Mesoscale Model (MM5). Part I: Model description and first results (2005, background): “Each type of cloud particle/hydrometeor is described using size (mass) distribution functions containing several tens of bins of masses (e.g., Khvorostyanov et al. 1989; Hall 1980; Reisin et al. 1996; Ovtchinnikov and Kogan 2000; Yin et al. 2000; Rasmussen et al. 2002 ).”