Ice particles in stratiform clouds in the Arctic and possible mechanisms for the production of high ice concentrations

By A. Rangno, P. Hobbs. 2001

187 citations recorded by the source corpus.

Subfields: Atmospheric Science, Earth-Surface Processes, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/a1a6e476de7c18156f7e3a4cd7438ec4ebbbac41

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Citations in the corpus

Mesoscale modeling of springtime Arctic mixed-phase stratiform clouds using a new two-moment bulk microphysics scheme (2005, background): “Droplet and ice crystal concentrations and sizes are particularly important in supercooled arctic clouds (e.g., Hobbs and Rangno 1998; Rangno and Hobbs 2001; Pinto 1998; Pinto et al. 2001; Harrington et al. 1999).”
Observations of ice multiplication in a weakly convective cell embedded in supercooled mid-level stratus (2010, background): “The HM process has been identiﬁed in several other studies as being an important mechanism for accounting for observed ice crystal concentrations ( Blyth and Latham, 1997; Rangno and Hobbs, 2001; Hogan et al., 2002).”
Secondary Ice Production: Current State of the Science and Recommendations for the Future (2016, unknown): “There are also observations to suggest that large ice crystal number concentrations occur in frontal (e.g., Crosier et al. 2011) and super-cooled boundary layer stratus cloud (e.g., Rangno and Hobbs 2001).”
Confronting the Challenge of Modeling Cloud and Precipitation Microphysics (2020, background): “…sampling similar cloud systems can be aggregated, basic process occurrence can be systematically investigated in the greatest detail (e.g., Rangno & Hobbs, 2001), including individual ice crystal morphologies and hydrometeor SD features that bear direct evidence of ice formation, vapor growth,…”
Arctic Mixed-Phase Cloud Properties from AERI Lidar Observations: Algorithm and Results from SHEBA (2005, background): “The lack of the larger water droplets in the mixed-phase clouds, which results in a shift to a smaller effective radius, may be due to the larger droplets being removed from the size distribution because the larger droplets are more likely to freeze (Rangno and Hobbs 2001).”
Mixed-Phase Clouds: Progress and Challenges (2017, background): “…by inhibiting riming growth (Borys et al. 2003); and (iii) a cold second indirect effect, where increases in CCN increase the droplet number concentration, decrease liquid drop sizes, and inhibit ice crystal formation through less efficient secondary ice crystal production (Rangno and Hobbs 2001).”
Evidence of liquid dependent ice nucleation in high‐latitude stratiform clouds from surface remote sensors (2011, result): “The idea of liquid‐dependent ice nucleation also supports work by Rangno and Hobbs [2001] who demonstrated a relationship between ice concentration and droplet threshold diameter for Arctic clouds.”