Deposition ice nucleation on soot at temperatures relevant for the lower troposphere
By Magdalena Dymarska, B. Murray, Limin Sun, M. Eastwood, D. Knopf, A. Bertram. 2006
160 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/97e8c9b22b148863f908ae6de0e9fd3f4b887541
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In Atmospheric Science
In Global and Planetary Change
Citations in the corpus
- A Classical-Theory-Based Parameterization of Heterogeneous Ice Nucleation by Mineral Dust, Soot, and Biological Particles in a Global Climate Model (2010, background): “We note that the efficiency of soot deposition nucleation above 2388C is a matter of debate in recent literature (Gorbunov et al. 2001; Dymarska et al. 2006).”
- Deactivation of ice nuclei due to atmospherically relevant surface coatings (2009, background): “Other particles, for example carbonaceous cores from biomass burning and fossil fuel combustion, are more atmospherically common (Murphy et al 2006) but less effective as IN (DeMott et al 2003a, Dymarska et al 2006).”
- Enhanced Solar Energy Absorption by Internally-Mixed Black Carbon in Snow Grains (2012, background): “Like most particles, BC nucleates ice very poorly via direct deposition of vapor (e.g.,Dymarska et al., 2006), so most relevant mechanisms involve liquid water.”
- Heterogeneous freezing of ice on atmospheric aerosols containing ash, soot, and soil (2009, unknown): “Upon emission, soot is an insoluble and extremely hydrophobic substance and a poor IN [ DeMott , 1990; Wyslouzil et al. , 1994; Gorbunov et al. , 2001; Dymarska et al. , 2006].”
- Ice nuclei emissions from biomass burning (2009, background): “Laboratory studies have considered ice nucleation on several types of soot particles [DeMott, 1990; Diehl and Mitra, 1998; Dymarska et al., 2006; Gorbunov et al., 2001] and found that combustion soot is unlikely to undergo deposition ice nucleation but suggested a potential for combustion soot”