Heavy snowfall event over the Swiss Alps: did wind shear impact secondary ice production?

Abstract K dp > 1 ∘  km- 1 - 15  ∘ C suggested that a large population of oblate ice particles was present in the atmosphere. Here, we show that ice–graupel collisions are a likely origin of this population, probably enhanced by turbulence. We perform sensitivity simulations that include ice–graupel collisions of a cold frontal passage to investigate whether these simulations can capture the event better and whether the vertical wind shear had an impact on the secondary ice production (SIP) rate. The simulations are conducted with the Consortium for Small-scale Modeling (COSMO), at a 1 km horizontal grid spacing in the Davos region in Switzerland. The rime-splintering simulations could not reproduce the high ice crystal number concentrations, produced too large ice particles and therefore overestimated the radar reflectivity. The collisional-breakup simulations reproduced both the measured horizontal reflectivity and the ground-based observations of hydrometeor number concentration more accurately (∼ 20  L- 1). During 14:30–15:45 UTC the vertical wind shear strengthened by 60 % within the region favorable for SIP. Calculation of the mutual information between the SIP rate and vertical wind shear and updraft velocity suggests that the SIP rate is best predicted by the vertical wind shear rather than the updraft velocity. The ice–graupel simulations were insensitive to the parameters in the model that control the size threshold for the conversion from ice to graupel and snow to graupel.

Standort
Deutsche Nationalbibliothek Frankfurt am Main
Umfang
Online-Ressource
Sprache
Englisch

Erschienen in
Heavy snowfall event over the Swiss Alps: did wind shear impact secondary ice production? ; volume:23 ; number:4 ; year:2023 ; pages:2345-2364 ; extent:20
Atmospheric chemistry and physics ; 23, Heft 4 (2023), 2345-2364 (gesamt 20)

Urheber
Dedekind, Zane
Grazioli, Jacopo
Austin, Philip H.
Lohmann, Ulrike

DOI
10.5194/acp-23-2345-2023
URN
urn:nbn:de:101:1-2023033006510932491520
Rechteinformation
Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
Letzte Aktualisierung
14.08.2025, 10:55 MESZ

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