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    Estimating Surface Attachment Kinetic and Growth Transition Influences on Vapor-Grown Ice Crystals

    Source: Journal of the Atmospheric Sciences:;2020:;volume( 77 ):;issue: 007::page 2393
    Author:
    Pokrifka, Gwenore F.;Moyle, Alfred M.;Hanson, Lavender Elle;Harrington, Jerry Y.
    DOI: 10.1175/JAS-D-19-0303.1
    Publisher: American Meteorological Society
    Abstract: There are few measurements of the vapor growth of small ice crystals at temperatures below −30°C. Presented here are mass-growth measurements of heterogeneously and homogeneously frozen ice particles grown within an electrodynamic levitation diffusion chamber at temperatures between −44° and −30°C and supersaturations si between 3% and 29%. These growth data are analyzed with two methods devised to estimate the deposition coefficient α without the direct use of si. Measurements of si are typically uncertain, which has called past estimates of α into question. We find that the deposition coefficient ranges from 0.002 to unity and is scattered with temperature, as shown in prior measurements. The data collectively also show a relationship between α and si, with α rising (falling) with increasing si for homogeneously (heterogeneously) frozen ice. Analysis of the normalized mass growth rates reveals that heterogeneously frozen crystals grow near the maximum rate at low si, but show increasingly inhibited (low α) growth at high si. Additionally, 7 of the 17 homogeneously frozen crystals cannot be modeled with faceted growth theory or constant α. These cases require the growth mode to transition from efficient to inefficient in time, leading to a large decline in α. Such transitions may be, in part, responsible for the inconsistency in prior measurements of α.
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      Estimating Surface Attachment Kinetic and Growth Transition Influences on Vapor-Grown Ice Crystals

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    contributor authorPokrifka, Gwenore F.;Moyle, Alfred M.;Hanson, Lavender Elle;Harrington, Jerry Y.
    date accessioned2022-01-30T17:50:23Z
    date available2022-01-30T17:50:23Z
    date copyright6/12/2020 12:00:00 AM
    date issued2020
    identifier issn0022-4928
    identifier otherjasd190303.pdf
    identifier urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4264027
    description abstractThere are few measurements of the vapor growth of small ice crystals at temperatures below −30°C. Presented here are mass-growth measurements of heterogeneously and homogeneously frozen ice particles grown within an electrodynamic levitation diffusion chamber at temperatures between −44° and −30°C and supersaturations si between 3% and 29%. These growth data are analyzed with two methods devised to estimate the deposition coefficient α without the direct use of si. Measurements of si are typically uncertain, which has called past estimates of α into question. We find that the deposition coefficient ranges from 0.002 to unity and is scattered with temperature, as shown in prior measurements. The data collectively also show a relationship between α and si, with α rising (falling) with increasing si for homogeneously (heterogeneously) frozen ice. Analysis of the normalized mass growth rates reveals that heterogeneously frozen crystals grow near the maximum rate at low si, but show increasingly inhibited (low α) growth at high si. Additionally, 7 of the 17 homogeneously frozen crystals cannot be modeled with faceted growth theory or constant α. These cases require the growth mode to transition from efficient to inefficient in time, leading to a large decline in α. Such transitions may be, in part, responsible for the inconsistency in prior measurements of α.
    publisherAmerican Meteorological Society
    titleEstimating Surface Attachment Kinetic and Growth Transition Influences on Vapor-Grown Ice Crystals
    typeJournal Paper
    journal volume77
    journal issue7
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/JAS-D-19-0303.1
    journal fristpage2393
    journal lastpage2410
    treeJournal of the Atmospheric Sciences:;2020:;volume( 77 ):;issue: 007
    contenttypeFulltext
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