Limitations of the Wegener–Bergeron–Findeisen Mechanism in the Evolution of Mixed-Phase Clouds
By A. Korolev. 2007
286 citations recorded by the source corpus.
Subfields: Atmospheric Science, Earth-Surface Processes, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/ace7a7ef5f1fb83952674665b79485fc8a0d2ef7
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Citations in the corpus
- Sensitivity studies of different aerosol indirect effects in mixed-phase clouds (2009, methodology): “Another difference between the ECHAM version used in this study and that described in Lohmann et al.(2008) is that this version includes the aerosol-size dependent belowcloud scavenging byCroft et al.”
- Improvements to an Empirical Parameterization of Heterogeneous Ice Nucleation and Its Comparison with Observations (2013, methodology): “In mixed-phase cloud, the humidity is maintained close to water saturation by the liquid phase (Korolev and Mazin 2003; Korolev 2007).”
- A microphysics guide to cirrus – Part 2: Climatologies of clouds and humidity from observations (2020, background): “This is because the high updrafts keep both RHw and RHice above 100 %, and thus the Wegener–Bergeron–Findeisen process does not take place (Korolev, 2007).”
- Mixed-Phase Clouds: Progress and Challenges (2017, methodology): “Korolev (2007) shows typical digital images of spherical particles as a function of distance from the object plane using an OAP (Fig.”
- Overview of Ice Nucleating Particles (2017, background): “In mixed-phase clouds (MPCs) the role of ice crystals is particularly important because ice can in-fluence the supercooled liquid water content through the Wegener–Bergeron–Findeisen process (Korolev 2007; Korolev and Field 2008).”
- Review of Aerosol–Cloud Interactions: Mechanisms, Significance, and Challenges (2016, background): “However, the WBF process can only occur under a limited range of conditions because it requires that the vapor pressure exceeds ice saturation but is below liquid saturation (Korolev 2007; Korolev and Mazin 2003).”