2021
DOI: 10.5194/acp-2021-511
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Aerosol-cloud interactions: The representation of heterogeneous ice activation in cloud models

Abstract: Abstract. The homogeneous nucleation of ice in supercooled liquid water clouds is characterized by time-dependent freezing rates. By contrast, water phase transitions induced heterogeneously by ice nucleating particles (INPs) are described by time-independent ice-active fractions depending on ice supersaturation (s). Laboratory studies report ice-active particle number fractions (AFs) that are cumulative in s. Cloud models budget INP and ice crystal numbers to conserve total particle number during water phase … Show more

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Cited by 2 publications
(9 citation statements)
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“…A common method to simulate the number of ice crystals that form from a heterogeneous nucleation event is based on the AF of available INPs. This quantity is derived from cloud or continuous flow chamber experiments of the number of frozen particles (Kärcher and Marcolli, 2021). Vali (1971) and Vali (2019) defined two approaches for determining the number of INPs that become ice active.…”
Section: Introductionmentioning
confidence: 99%
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“…A common method to simulate the number of ice crystals that form from a heterogeneous nucleation event is based on the AF of available INPs. This quantity is derived from cloud or continuous flow chamber experiments of the number of frozen particles (Kärcher and Marcolli, 2021). Vali (1971) and Vali (2019) defined two approaches for determining the number of INPs that become ice active.…”
Section: Introductionmentioning
confidence: 99%
“…On the other hand, the latter approach can be used to determine the ice nucleation ability of a population of particles, which is relevant to modeling cirrus ice formation processes that can occur on numerous particles. However, as Kärcher and Marcolli (2021) highlight, care must be taken when determining which approach to use when calculating the number of ice crystals that can form on INPs. For example, if a model explicitly removes INPs from the total available population after each ice formation event and adds them to the newly nucleated ice number concentrations (i.e.…”
Section: Introductionmentioning
confidence: 99%
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