Evaporation freezing by contact nucleation inside‐out

By A. Durant, Raymond A. Shaw. 2005

178 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/2dd4a2a7db0442e0e4931f5683c8e5573393891e

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Citations in the corpus

Overview of Ice Nucleating Particles (2017, background): “1-1 (Durant and Shaw 2005; Fornea et al. 2009; Shaw et al. 2005).”
A comprehensive laboratory study on the immersion freezing behavior of illite NX particles. A comparison of 17 ice nucleation measurement techniques (2014, background): “These heterogeneous ice formation processes include deposition nucleation, immersion freezing, condensation freezing, and contact freezing (Vali, 1985), inside-out contact freezing (i.e., freezing of an immersed INP in contact with the droplet surface from the inside; Durant and Shaw, 2005; Fornea e”
Representation of microphysical processes in cloud‐resolving models: Spectral (bin) microphysics versus bulk parameterization (2015, methodology): “Laboratory experiments on ice nucleation [Roberts and Hallett, 1967; Durant and Shaw, 2005], secondary ice nucleation [Hallett and Mossop, 1974], efficiency of collisions, aerosol scavenging and riming [Mitra et al., 1990, 1992], turbulent effects on droplet growth [Vohl et al., 1999],…”
In Situ Observations of the Microphysical Properties of Wave, Cirrus, and Anvil Clouds. Part II: Cirrus Clouds (2006, background): “The sudden increase in ice concentration at the glaciation transition point may be due to a recently discovered phenomenon: that contact nucleation is effective from inside droplets as well as via dry particles making contact from outside droplets (Shaw et al. 2005; Durant and Shaw 2005).”
Experimental study on the ice nucleation ability of size-selected kaolinite particles in the immersion mode (2010, methodology): “tant for the understanding of precipitation formation and of cloud radiative properties [e.g., Ansmann et al., 2008; Cantrell and Heymsfield, 2005; Durant and Shaw, 2005].”
Improvements to an Empirical Parameterization of Heterogeneous Ice Nucleation and Its Comparison with Observations (2013, background): “Contact freezing seen by Durant and Shaw (2005) and Shaw et al. (2005) might have been favored because of solid roughness, which could have allowed solid contact with the liquid surface away from the line.”
Heterogeneous freezing of ice on atmospheric aerosols containing ash, soot, and soil (2009, unknown): “…out, measurements focused specifically on contact freezing are needed [ DeMott , 1995; Kanji and Abbatt , 2006; Pant et al. , 2006; Durant et al. , 2008; Eastwood et al. , 2008; Knopf and Koop , 2008; Mo¨hler et al. , 2006; Diehl and Mitra , 1998; Durant and Shaw , 2005; Shaw et al. , 2005].”
Ice structures, patterns, and processes: A view across the icefields (2012, background): “The freezing temperatures of evaporating droplets have been elevated up to four degrees as immersed solid particles come into contact with the surface (Durant and Shaw, 2005).”
A Classical-Theory-Based Parameterization of Heterogeneous Ice Nucleation by Mineral Dust, Soot, and Biological Particles in a Global Climate Model (2010, background): “Other less well-understood freezing mechanisms (e.g., inside-out contact nucleation; Durant and Shaw 2005) are not considered here.”
Review of Aerosol–Cloud Interactions: Mechanisms, Significance, and Challenges (2016, background): “For example, laboratory experiments on ice nucleation (Durant and Shaw 2005; Niemand et al. 2012), secondary ice formation (Hallett and Mossop 1974), efficiency of collisions, and aerosol scavenging and riming (Mitra et al. 1990, 1992) have substantially contributed to our knowledge of…”