The deposition ice nucleation and immersion freezing potential of amorphous secondary organic aerosol: Pathways for ice and mixed‐phase cloud formation

By Bingbing Wang, A. Lambe, P. Massoli, T. Onasch, P. Davidovits, D. Worsnop, D. Knopf. 2012

180 citations recorded by the source corpus.

How researchers see this paper

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

Overview of Ice Nucleating Particles (2017, background): “Therefore, it is not surprising that varied ice nucleating activity of organic particles results from the different types of SOA investigated, variable organic composition, and corresponding viscosity of the aerosol particles and particle-generation methods used.”
Competition between water uptake and ice nucleation by glassy organic aerosol particles (2014, methodology): “For SOA, deposition freezing data on naphthalene SOA from Wang et al. (2012) (red downward triangles) as well as nucleation data on aqSOA from Schill et al. (2014) (pink upward triangles) are used.”
Predicting the glass transition temperature and viscosity of secondary organic material using molecular composition (2017, background): “…et al., 2014; Price et al., 2014), affecting homogeneous vs. heterogeneous ice nucleation pathways (Murray et al., 2010; Wagner et al., 2012; Wang et al., 2012a, b; Wilson et al., 2012; Baustian et al., 2013; Schill and Tolbert, 2013; Berkemeier et al., 2014; Schill et al., 2014; Lienhard…”