Growth Rates and Habits of Ice Crystals between −20° and −70°C

By M. Bailey, J. Hallett. 2004

226 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/0fad7514c882dbbc37f24a2476864bd4b69e3a30

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Citations in the corpus

The physics of snow crystals (2005, background): “Note that the morphology diagram in figure 2 is not necessarily indicative of all natural snow crystals, which are often dominated by polycrystalline forms, but rather it reflects the growth of ice single-crystals [21].”
Modelling of cirrus clouds – Part 1a: Model description and validation (2008, methodology): “Generally, we assume that ice crystals are hexagonal columns (Bailey and Hallet, 2004), with height L and diameter D (twice the side length of the hexagon). The aspect ratio ra : =L/D depends on crystal size, such that small crystals have ra=1 and larger crystals have ra>1. Mass-length relations fro”
Ice structures, patterns, and processes: A view across the icefields (2012, background): “Field and laboratory studies have continued through to the present in an attempt to assess more accurately the effect of varying thermodynamic parameters and the process of nucleation (e.g., Bailey and Hallett, 2004; Furukawa and Nada, 1997b).”
In Situ Observations of the Microphysical Properties of Wave, Cirrus, and Anvil Clouds. Part II: Cirrus Clouds (2006, background): “These observations are in agreement with the laboratory findings of Bailey and Hallett (2004). The particles in cirrus clouds tend to fall into crystal habit categories that are a function of particle size.”
A large‐eddy model for cirrus clouds with explicit aerosol and ice microphysics and Lagrangian ice particle tracking (2010, background): “Recent laboratory studies (Bailey and Hallett, 2004, 2009) have addressed this issue.”
A Comprehensive Habit Diagram for Atmospheric Ice Crystals: Confirmation from the Laboratory, AIRS II, and Other Field Studies (2009, background): “Since 2004, a comprehensive picture of atmospheric ice crystal behavior has been revealed through both laboratory studies (Bailey and Hallett 2002, 2004, hereafter BH02 and BH04) and field observations utilizing the Spec.”
Confronting the Challenge of Modeling Cloud and Precipitation Microphysics (2020, background): “For instance, the measurements of Bailey and Hallett (2004) provide a wealth of data on ice crystal shapes along with axis and volume growth rates, but it is not clear how these empirical axis‐dependent growth rates can be used in numerical models that use simplified mass growth equations based on…”