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Ice-Ice Collisions: An Ice Multiplication Process in Atmospheric Clouds

Yano, J. -I. and Phillips, Vaughan LU (2011) In Journal of Atmospheric Sciences 68(2). p.322-333
Abstract
Ice in atmospheric clouds undergoes complex physical processes, interacting especially with radiation, which leads to serious impacts on global climate. After their primary production, atmospheric ice crystals multiply extensively by secondary processes. Here, it is shown that a mostly overlooked process of mechanical breakup of ice particles by ice-ice collisions contributes to such observed multiplication. A regime for explosive multiplication is identified in its phase space of ice multiplication efficiency and number concentration of ice particles. Many natural mixed-phase clouds, if they have copious millimeter-sized graupel, fall into this explosive regime. The usual Hallett-Mossop (H-M) process of ice multiplication is shown to... (More)
Ice in atmospheric clouds undergoes complex physical processes, interacting especially with radiation, which leads to serious impacts on global climate. After their primary production, atmospheric ice crystals multiply extensively by secondary processes. Here, it is shown that a mostly overlooked process of mechanical breakup of ice particles by ice-ice collisions contributes to such observed multiplication. A regime for explosive multiplication is identified in its phase space of ice multiplication efficiency and number concentration of ice particles. Many natural mixed-phase clouds, if they have copious millimeter-sized graupel, fall into this explosive regime. The usual Hallett-Mossop (H-M) process of ice multiplication is shown to dominate the overall ice multiplication when active, as it starts sooner, compared to the breakup ice multiplication process. However, for deep clouds with a cold base temperature where the usual H-M process is inactive, the ice breakup mechanism should play a critical role. Supercooled rain, which may freeze to form graupel directly in only a few minutes, is shown to hasten such ice multiplication by mechanical breakup, with an ice enhancement ratio exceeding 10(4) approximately 20 min after small graupel first appear. The ascent-dependent onset of subsaturation with respect to liquid water during explosive ice multiplication is predicted to determine the eventual ice concentrations. (Less)
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author
publishing date
type
Contribution to journal
publication status
published
subject
in
Journal of Atmospheric Sciences
volume
68
issue
2
pages
322 - 333
publisher
Amer Meteorological Soc
external identifiers
  • wos:000288144300009
  • scopus:79953188395
ISSN
1520-0469
DOI
10.1175/2010JAS3607.1
language
English
LU publication?
no
id
5d29a87f-7503-416d-9bb6-38d24a3c6a1b (old id 4587455)
date added to LUP
2014-08-15 10:29:26
date last changed
2017-11-19 03:14:29
@article{5d29a87f-7503-416d-9bb6-38d24a3c6a1b,
  abstract     = {Ice in atmospheric clouds undergoes complex physical processes, interacting especially with radiation, which leads to serious impacts on global climate. After their primary production, atmospheric ice crystals multiply extensively by secondary processes. Here, it is shown that a mostly overlooked process of mechanical breakup of ice particles by ice-ice collisions contributes to such observed multiplication. A regime for explosive multiplication is identified in its phase space of ice multiplication efficiency and number concentration of ice particles. Many natural mixed-phase clouds, if they have copious millimeter-sized graupel, fall into this explosive regime. The usual Hallett-Mossop (H-M) process of ice multiplication is shown to dominate the overall ice multiplication when active, as it starts sooner, compared to the breakup ice multiplication process. However, for deep clouds with a cold base temperature where the usual H-M process is inactive, the ice breakup mechanism should play a critical role. Supercooled rain, which may freeze to form graupel directly in only a few minutes, is shown to hasten such ice multiplication by mechanical breakup, with an ice enhancement ratio exceeding 10(4) approximately 20 min after small graupel first appear. The ascent-dependent onset of subsaturation with respect to liquid water during explosive ice multiplication is predicted to determine the eventual ice concentrations.},
  author       = {Yano, J. -I. and Phillips, Vaughan},
  issn         = {1520-0469},
  language     = {eng},
  number       = {2},
  pages        = {322--333},
  publisher    = {Amer Meteorological Soc},
  series       = {Journal of Atmospheric Sciences},
  title        = {Ice-Ice Collisions: An Ice Multiplication Process in Atmospheric Clouds},
  url          = {http://dx.doi.org/10.1175/2010JAS3607.1},
  volume       = {68},
  year         = {2011},
}