1976
DOI: 10.1175/1520-0469(1976)033<1995:tsoipf>2.0.co;2
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The Survival of Ice Particles Falling from Cirrus Clouds in Subsaturated Air

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Cited by 187 publications
(174 citation statements)
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“…The heat balance of an ice crystal in a rarefied atmosphere is represented by the following form (Hall and Pruppacher, 1976;Roach, 1976;Stephens, 1983;Hallett, 1987;Hallett et al, 2002):…”
Section: Heat Balance Of An Ice Crystalmentioning
confidence: 99%
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“…The heat balance of an ice crystal in a rarefied atmosphere is represented by the following form (Hall and Pruppacher, 1976;Roach, 1976;Stephens, 1983;Hallett, 1987;Hallett et al, 2002):…”
Section: Heat Balance Of An Ice Crystalmentioning
confidence: 99%
“…where T s and T e refer to the ice crystal surface and the environmental air temperature, respectively; ρ v and ρ si denote the density of the ambient water vapour and saturated water vapour near a crystal, respectively; S denotes crystal surface area; f m and f Q are the ventilation factors expressed in Hall and Pruppacher (1976). Other factors are:…”
Section: Heat Balance Of An Ice Crystalmentioning
confidence: 99%
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“…The effective fall speed can be further reduced by mesoscale rising motion and/or convective lofting associated with the cirrus clouds themselves. Crystals are capable of surviving for extended periods as they fall through subsaturated air (e.g., Hall and Pruppacher, 1976).…”
Section: Prognostic Cloud Variablesmentioning
confidence: 99%