Heterogeneous nucleation of ice on surrogates of mineral dust
By D. Knopf, Thomas Koop. 2006
175 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/4aed3c0f3f3a976efbf013fde37dc528a30204e3
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Citations in the corpus
- Experimental study on the ice nucleation ability of size-selected kaolinite particles in the immersion mode (2010, background): “have shown mineral dust particles to be active as INs in the deposition mode [e.g., Eastwood et al., 2008; Knopf and Koop, 2006; Mohler et al., 2006; Kanji et al., 2008; Archuleta et al., 2005; Welti et al., 2009].”
- The deposition ice nucleation and immersion freezing potential of amorphous secondary organic aerosol: Pathways for ice and mixed‐phase cloud formation (2012, background): “Whereas for the mineral dust, such as Arizona test dust [Knopf and Koop, 2006] and Kaolinite [Knopf et al., 2010;Wang and Knopf, 2011] deposition ice nucleation was, for the majority of the cases, initiated by the same particle when the ice nucleation experiments were repeated at the same…”
- Overview of Ice Nucleating Particles (2017, methodology): “Knopf and Koop (2006) used ATD particles to show that such so-called ice preactivation is relevant for dust if the condition of subzero temperatures between cycles is maintained yielding a 10%–30% lower onset RH i .”
- A Classical-Theory-Based Parameterization of Heterogeneous Ice Nucleation by Mineral Dust, Soot, and Biological Particles in a Global Climate Model (2010, background): “ious other parameters has been the subject of numerous laboratory experiments (e.g., Schaller and Fukuta 1979; Levin and Yankofsky 1983; Knopf and Koop 2006; Bundke et al. 2008; Durant et al. 2008; Welti et al. 2009).”
- Deactivation of ice nuclei due to atmospherically relevant surface coatings (2009, methodology): “In agreement with the finding of Archuleta et al (2005) for aluminum oxide, but contrary to the findings of Eastwood et al (2009), Knopf and Koop (2006) found little or no coating effect on IN potential.”
- A large‐eddy model for cirrus clouds with explicit aerosol and ice microphysics and Lagrangian ice particle tracking (2010, background): “1 or more) (Möhler, et al., 2006; Knopf and Koop, 2006), indicative of variability in IN surface properties or chemical composition of individual dust IN particles.”
- 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].”