The Impact of Hail Size on Simulated Supercell Storms

By S. C. Heever, William Cotton. 2004

170 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/1b4136c4dcabd0abe726b446d9037955a2dad33a

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Citations in the corpus

Aerosol Indirect Effects on Tropical Convection Characteristics under Conditions of Radiative-Convective Equilibrium (2011, background): “…et al. 2007). e. Dynamic response to AIF Variations in the cloud microphysics through enhanced aerosol concentrations have previously been observed to have an impact on the storm dynamics (van den Heever and Cotton 2004; Khain et al. 2005; Seifert and Beheng 2006; van den Heever and Cotton 2007).”
Tornadogenesis: Our current understanding, forecasting considerations, and questions to guide future research (2009, background): “…of microphysical differences among supercells and how those microphysical differences arise (Tartaglione et al., 1996; Gilmore et al., 2004; van den Heever and Cotton, 2004), the thermodynamic characteristics of supercells above the ground, the effects of radiative transfer processes on storm…”
Comparison of Two-Moment Bulk Microphysics Schemes in Idealized Supercell Thunderstorm Simulations (2011, methodology): “For example, Gilmore et al. (2004) and Van Weverberg et al. (2010) showed large sensitivity of simulated supercell storm dynamics and precipitation to changes in the assumed bulk density and fixed intercept parameter of the graupel/hail category using single-moment BMSs. Similarly, van den Heever…”
Confronting the Challenge of Modeling Cloud and Precipitation Microphysics (2020, background): “…of simulations to how ice is partitioned among categories and to the bulk properties assumed for a given category (e.g., Adams‐Selin et al., 2013; Bryan & Morrison, 2012; McCumber et al., 1991; Morrison & Milbrandt, 2011; van den Heever & Cotton, 2004; van Weverberg et al., 2012; and many others).”
Evaluation of cloud‐resolving and limited area model intercomparison simulations using TWP‐ICE observations: 1. Deep convective updraft properties (2014, result): “…have the smallest rimed ice mixing ratios (Figure 11d) and greatest snow-mixing ratios (Figure 11e) in the upper troposphere, which is consistent with results in several other studies [Gilmore et al., 2004; van den Heever and Cotton, 2004; Morrison andMilbrandt, 2011; VanWeverberg et al., 2012].”
Representation of microphysical processes in cloud‐resolving models: Spectral (bin) microphysics versus bulk parameterization (2015, background): “252 and Cotton, 2004, 2008; van den Heever and Cotton, 2004, 2007; Carrió et al., 2007; van den Heever et al., 2006, 2011; Seigel and van den Heever, 2012; Storer and van den Heever, 2013; Igel et al., 2013; Saleeby and van den Heever, 2013].”
Developments in the CSU-RAMS Aerosol Model: Emissions, Nucleation, Regeneration, Deposition, and Radiation (2013, unknown): “It has demonstrated success in simulating a range of atmospheric phenomena, such as supercell thunderstorms (e.g., van den Heever and Cotton 2004), mesoscale convective systems (e.g., Olsson and Cotton 1997; Bernardet and Cotton 1998), mixed-phase orographic precipitation (Saleeby et al. 2009,…”
A review on regional convection‐permitting climate modeling: Demonstrations, prospects, and challenges (2015, background): “It is not clear if introducing graupel or hail weakens [Van Den Heever and Cotton, 2004; Cohen and McCaul, 2006; Adams-Selin et al., 2013] or strengthens [Van Weverberg et al., 2011, 2012; Morrison and Milbrandt, 2010] cold pools formed from thunderstorm outflows.”
Comparison of Evaporation and Cold Pool Development between Single-Moment and Multimoment Bulk Microphysics Schemes in Idealized Simulations of Tornadic Thunderstorms (2010, background): “It is known that variations in the hail category have a strong impact on storm simulations (Gilmore et al. 2004; van den Heever and Cotton 2004).”
Modeling Aerosol Impacts on Convective Storms in Different Environments (2009, background): “A number of other studies (e.g., van den Heever and Cotton 2004; Lerach et al. 2008) have successfully simulated convective storms using a temperature perturbation of similar magnitude.”