Spectral (Bin) Microphysics Coupled with a Mesoscale Model (MM5). Part II: Simulation of a CaPE Rain Event with a Squall Line

By Barry H. Lynn, Alexander Khain, Jimy Dudhia, Daniel Rosenfeld, Andrei Pokrovsky, A. Seifert. 2005

146 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/292097c117ace51712cea3567e867d6971a37432

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Citations in the corpus

Aerosol Effects on Intensity of Landfalling Hurricanes as Seen from Simulations with the WRF Model with Spectral Bin Microphysics (2010, background): “…accurate than the bulk parameterization with regard to its ability to simulate cloud dynamics and microphysics and precipitation (see comparisons of SBM versus bulk schemes in Lynn et al. 2005b; Lynn and Khain 2007; Li et al. 2009a,b; Iguchi et al. 2008; Khain and Lynn 2009; Khain et al. 2009).”
Notes on state-of-the-art investigations of aerosol effects on precipitation: a critical review (2009, methodology): “…schemes have a significant advantage as compared to the bulk schemes, because they calculate the changes in the size distributions caused by aerosols (Lynn et al 2005b, Li et al 2008b), and take into account the change in the aerosol concentration and size distribution during nucleation.”
A Comparison of TWP-ICE Observational Data with Cloud-Resolving Model Results (2012, result): “The simulated degree of linear organization can in turn be substantially modified by microphysics (e.g., DHARMA-1 versus DHARMA-2M), consistent with past modeling results [e.g., Lynn et al., 2005].”
Spectral (Bin) microphysics coupled with a Mesoscale Model (MM5). Part I: Model description and first results (2005, background): “Supplemental simulations (see Lynn et al. 2005, hereafter Part II) show that the Reisner2 scheme produced the best agreement between precipitation amount and observed precipitation.”
A two-moment cloud microphysics parameterization for mixed-phase clouds. Part 2: Maritime vs. continental deep convective storms (2006, background): “Recently some results of bin microphysical mixed-phase schemes in 3-D models have been presented by Ovtchinnikov and Kogan (2000) as well as Lynn et al (2005a; 2005b) .”
Aerosol impact on the dynamics and microphysics of deep convective clouds (2005, methodology): “Simulations with the spectral microphysics MM5 model (Lynn et al. 2005b) of a rain event over Florida accompanied by a squall-line formation showed that the increase in the CCN concentration led to some decrease in the net precipitation amount over the area with linear sizes of several hundred…”