Ice particle habits in stratiform clouds

By A. Korolev, George Isaac, J. Hallett. 2000

161 citations recorded by the source corpus.

Subfields: Aerospace Engineering, Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/a6919da4c06bb6325f0fffb34f4eee1f60795f97

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Aerospace Engineering

1. Anthony J. Baran
2. J. Hallett
3. Paul R. Field
4. Robin J. Hogan
5. A. Bansemer
6. T. Bartels-Rausch
7. A. Korolev
8. George Isaac

In Atmospheric Science

1. Anthony J. Baran
2. Andrew J. Heymsfield
3. A. Bansemer
4. Paul R. Field
5. Robin J. Hogan
6. T. Bartels-Rausch
7. A. Korolev
8. J. Hallett

In Global and Planetary Change

1. Anthony J. Baran
2. Andrew J. Heymsfield
3. A. Bansemer
4. Paul R. Field
5. A. Korolev
6. Robin J. Hogan
7. T. Bartels-Rausch
8. J. Hallett

Citations in the corpus

• A New Bulk Microphysical Scheme That Includes Riming Intensity and Temperature-Dependent Ice Characteristics (2011, background): “Ice particles have different properties and growth characteristics based on the ambient conditions (Korolev et al. 2000).”
• A review of the light scattering properties of cirrus (2009, background): “The hexagonal ice columns and plates are responsible for the appearance of the 221 and 461 halos, though these more pristine ice crystal shapes are not the most common [47,48].”
• Snow Size Distribution Parameterization for Midlatitude and Tropical Ice Clouds (2007, result): “1) for midlatitudes is between 5 and 10 L 1 in agreement with previous studies of midlatitude ice cloud (e.g., Korolev et al. 2000; Gultepe et al. 2001; Field et al. 2005; Boudala and Isaac 2006), while for the tropical data the mean is 10–50 L 1, again similar to previous independent measurements…”
• Parametrization of ice‐particle size distributions for mid‐latitude stratiform cloud (2005, background): “This is significant because many ice-nuclei parametrizations have increasing icenuclei concentration with decreasing temperature, as discussed by Korolev et al. (2000).”
• Observed Microphysical Structure of Midlevel, Mixed-Phase Clouds (2002, background): “Finally, Hobbs and Rangno (1998) and Korolev et al. (2000) previously showed that ice particle concentrations were poorly correlated with temperature.”
• Microphysical characterization of mixed‐phase clouds (2003, background): “However, the comparison of D3 in this study and Deff in the study of Korolev et al. (2000) provides indirect evidence that the FSSP gives a reasonable estimate of the concentration of ice particles in glaciated clouds.”
• A Comprehensive Habit Diagram for Atmospheric Ice Crystals: Confirmation from the Laboratory, AIRS II, and Other Field Studies (2009, background): “Inc. CPI (Lawson et al. 1998), a nonimpacting cloud particle imager.”
• Ice structures, patterns, and processes: A view across the icefields (2012, background): “Clouds are dynamic and may contain irregularly shaped particles consisting of faceted polycrystalline particles or smooth sublimating particles, as has been observed in Arctic cirrus and stratiform clouds (Korolev et al., 2000).”