Shattering during Sampling by OAPs and HVPS. Part I: Snow Particles

By A. Korolev, George Isaac. 2005

169 citations recorded by the source corpus.

Subfields: Earth-Surface Processes, Global and Planetary Change, Ocean Engineering

View Paper: https://www.semanticscholar.org/paper/001b0b263059b1b45cca4087e2f33f96f62557da

How researchers see this paper

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

In Earth-Surface Processes

1. R. P. Lawson
2. Paul R. Field
3. A. Bansemer
4. V. Phillips
5. M. Krämer
6. P. DeMott
7. C. Twohy
8. K. Prather

In Global and Planetary Change

1. R. P. Lawson
2. Andrew J. Heymsfield
3. A. Bansemer
4. C. Schmitt
5. Paul R. Field
6. C. Twohy
7. M. Krämer
8. V. Phillips

In Ocean Engineering

1. R. P. Lawson
2. Andrew J. Heymsfield
3. C. Schmitt
4. A. Bansemer
5. Paul R. Field
6. V. Phillips
7. A. Korolev
8. Anthony J. Baran

Citations in the corpus

• Cloud Ice Properties: In Situ Measurement Challenges (2017, background): “9.9 Unauthenticated | Downloaded 01/07/24 01:04 AM UTC fragments will be detected (Korolev and Isaac 2005; Korolev et al. 2011, 2013a; Field et al. 2006; Lawson 2011; Jackson et al. 2014; Korolev and Field 2015).”
• Shattering and Particle Interarrival Times Measured by Optical Array Probes in Ice Clouds (2006, background): “Korolev and Isaac (2005) concentrated on these probes in their analysis and looked at imagery of multiple particles within a single image frame and statistics associated with “zero interarrival time” particles.”
• Transport impacts on atmosphere and climate: Aviation (2009, unknown): “However, only a few measurements have attempted to quantify total ice crystal number in cirrus clouds, and the number of small particles is still controversial, since particle shattering within the inlet of airborne probes may cause over-counting (Korolev and Isaac, 2005; McFarquhar et al., 2007) .”
• Effects of ice particles shattering on the 2D-S probe (2011, methodology): “Cooper (1978) introduced the arrival time approach, which was later refined by Field et al. (2003, 2006), Korolev and Isaac (2005) and Baker et al. (2009).”
• Ice Cloud Particle Size Distributions and Pressure-Dependent Terminal Velocities from In Situ Observations at Temperatures from 0° to −86°C (2013, background): “The effects of shattering of ice particles on the leading surfaces of the probes designed to measure them (Gardiner and Hallett 1985; Korolev and Isaac 2005; Field et al. 2006; Heymsfield et al. 2008; Korolev et al. 2011) are discussed and evaluated when necessary.”
• Improvements to an Empirical Parameterization of Heterogeneous Ice Nucleation and Its Comparison with Observations (2013, background): “Yet this tends to be less important when ice particles are all smaller than 0.6 mm (Korolev and Isaac 2005), as seen in the simulated periods of ICE-”
• A Comprehensive Habit Diagram for Atmospheric Ice Crystals: Confirmation from the Laboratory, AIRS II, and Other Field Studies (2009, background): “…the idealized hexagonal shapes depicted in the habit diagrams, they have their own aesthetic appeal and are fascinating in their complexity, and it is time for a revised habit diagram that reflects these characteristics and the new revelations concerning habit, temperature, and ice supersaturation.”