A two-moment cloud microphysics parameterization for mixed-phase clouds. Part 2: Maritime vs. continental deep convective storms

By A. Seifert, Klaus D. Beheng. 2006

242 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/2f9fab7c560d51c1608f74b1d17699dbc89960e5

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Citations in the corpus

Sensitivity of a Simulated Squall Line to Horizontal Resolution and Parameterization of Microphysics (2012, unknown): “…schemes have also been widely used to treat droplet activation and cloud–aerosol interaction via prediction of the droplet number concentration (e.g., Ghan et al. 1997; Cohard and Pinty 2000; Morrison et al. 2005, hereafter M05; Seifert and Beheng 2006a,b; Phillips et al. 2007; Ming et al. 2007).”
Operational Convective-Scale Numerical Weather Prediction with the COSMO Model: Description and Sensitivities (2011, methodology): “In the following we present a sensitivity study comparing the operational Lin-type one-moment microphysics scheme described in section 2 with the more sophisticated two-moment scheme of Seifert and Beheng (2006a).”
Notes on state-of-the-art investigations of aerosol effects on precipitation: a critical review (2009, methodology): “…studies (e.g., Khain et al 2003, 2004, 2005, 2008a, Kaufman et al 2005, Lynn et al 2005a, 2005b, 2007, Lynn and Khain 2007, Matsui et al 2006, Seifert and Beheng 2006, Tao et al 2007, Lee et al 2005, 2008) it was shown that aerosol effects on the precipitation amount depend on the…”
Representation of microphysical processes in cloud‐resolving models: Spectral (bin) microphysics versus bulk parameterization (2015, methodology): “…time evolution of the moments of PSDs of collecting particles M kð Þx , collected particles M kð Þ y , and resulting hydrometeor M kð Þ z can be written as [Seifert and Beheng, 2006a] ∂M kð Þx ∂t xþy >z ¼ ∫ ∞ 0 ∫ ∞ 0 Kxyf x mxð Þf y my mkxdmxdmy (18) ∂M kð Þy ∂t ! xþy >z ¼ ∫ ∞ 0 ∫ ∞ 0 Kxyf x mxð…”
Parameterization of Cloud Microphysics Based on the Prediction of Bulk Ice Particle Properties. Part III: Introduction of Multiple Free Categories (2016, background): “…categories and up to three prognostic moments each in an attempt to model a greater range of particle types and processes (e.g., Straka and Mansell 2005; Milbrandt and Yau 2005a,b; Seifert and Beheng 2006; Thompson et al. 2008; Morrison et al. 2009; Mansell et al. 2010; Loftus et al. 2014).”
Development of an Effective Double-Moment Cloud Microphysics Scheme with Prognostic Cloud Condensation Nuclei (CCN) for Weather and Climate Models (2010, background): “However, the responses of aerosols on precipitation could be nonmonotonic and vary under different meteorological and aerosol conditions because of the complicated coupling between the cloud microphysics and dynamics (Seifert and Beheng 2006; Li et al. 2008).”
Aerosol Effects on Microstructure and Intensity of Tropical Cyclones (2012, background): “This added heat release invigorates the convection and often enhances rain amounts in a moist tropical atmosphere (Khain et al. 2005, 2008a,b; Seifert and Beheng 2006; van den Heever et al. 2006; van den Heever and Cotton 2007; Rosenfeld et al. 2008).”
Aerosol-cloud-precipitation effects over Germany as simulated by a convective-scale numerical weather prediction model (2011, methodology): “Seifert, A., Khain, A., Pokrovsky, A., and Beheng, K. D.: A comparison of spectral bin and two-moment bulk mixed-phase microphysics, Atmos.”
Global indirect aerosol effects: a review (2004, unknown): “More precipitation from polluted clouds was also simulated for different three-week periods over the Atmospheric Radiation Measurement Program (ARM) site in Oklahoma (Zhang et al., 2005) as well as for multicell cloud systems by (Seifert and Beheng, 2005).”
Modeling Aerosol Impacts on Convective Storms in Different Environments (2009, background): “In addition, differences in cloud type and environment can change the response (e.g., Matsui et al. 2004, 2006; Khain et al. 2005; Cohen and McCaul 2006; Seifert and Beheng 2006; Lynn et al. 2007; Lebsock et al. 2008; Khain 2009).”