Glass transition and phase state of organic compounds: dependency on molecular properties and implications for secondary organic aerosols in the atmosphere.

By Thomas Koop, Johannes Bookhold, M. Shiraiwa, Ulrich Pöschl. Physical Chemistry, Chemical Physics - PCCP, 2011

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Competition between water uptake and ice nucleation by glassy organic aerosol particles (2014, positive): “2 and 3, this time using the best guess parameters recommended in Koop et al. (2011).”
The deposition ice nucleation and immersion freezing potential of amorphous secondary organic aerosol: Pathways for ice and mixed‐phase cloud formation (2012, background): “DH2O at lower temperatures which results in slower diffusion of water molecules into the first particle layers [Koop et al., 2011; Shiraiwa et al., 2011; Zobrist et al., 2011] irrespec-”