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The Influence of Chemical and Mineral Compositions on the Parameterization of Immersion Freezing by Volcanic Ash Particles

Umo, N. S. ; Ullrich, R. ; Maters, E. C. ; Steinke, I. ; Benker, N. ; Höhler, K. ; Wagner, R. ; Weidler, P. G. ; Hoshyaripour, G. A. ; Kiselev, A. ; Kueppers, U. ; Kandler, K. ; Dingwell, D. B. ; Leisner, T. ; Möhler, O. (2024)
The Influence of Chemical and Mineral Compositions on the Parameterization of Immersion Freezing by Volcanic Ash Particles.
In: Journal of Geophysical Research: Atmospheres, 2021, 126 (17)
doi: 10.26083/tuprints-00020979
Artikel, Zweitveröffentlichung, Verlagsversion

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Kurzbeschreibung (Abstract)

Volcanic ash (VA) from explosive eruptions contributes to aerosol loadings in the atmosphere. Aside from the negative impact of VA on air quality and aviation, these particles can alter the optical and microphysical properties of clouds by triggering ice formation, thereby influencing precipitation and climate. Depending on the volcano and eruption style, VA displays a wide range of different physical, chemical, and mineralogical properties. Here, we present a unique data set on the ice nucleation activity of 15 VA samples obtained from different volcanoes worldwide. The ice nucleation activities of these samples were studied in the Aerosol Interaction and Dynamics in the Atmosphere (AIDA) cloud simulation chamber as well as with the Ice Nucleation Spectrometer of the Karlsruhe Institute of Technology (INSEKT). All VA particles nucleated ice in the immersion freezing mode from 263 to 238K with ice nucleation active site (INAS) densities ranging from ∼10⁵ to 10¹¹ m⁻², respectively. The variabilities observed among the VA samples, at any given temperature, range over 3.5 orders of magnitude. The ice‐nucleating abilities of VA samples correlate to varying degrees with their bulk pyroxene and plagioclase contents as a function of temperature. We combined our new data set with existing literature data to develop an improved ice nucleation parameterization for natural VA in the immersion freezing mode. This should be useful for modeling the impact of VA on clouds.

Typ des Eintrags: Artikel
Erschienen: 2024
Autor(en): Umo, N. S. ; Ullrich, R. ; Maters, E. C. ; Steinke, I. ; Benker, N. ; Höhler, K. ; Wagner, R. ; Weidler, P. G. ; Hoshyaripour, G. A. ; Kiselev, A. ; Kueppers, U. ; Kandler, K. ; Dingwell, D. B. ; Leisner, T. ; Möhler, O.
Art des Eintrags: Zweitveröffentlichung
Titel: The Influence of Chemical and Mineral Compositions on the Parameterization of Immersion Freezing by Volcanic Ash Particles
Sprache: Englisch
Publikationsjahr: 13 Februar 2024
Ort: Darmstadt
Publikationsdatum der Erstveröffentlichung: 2021
Ort der Erstveröffentlichung: Hoboken
Verlag: Wiley
Titel der Zeitschrift, Zeitung oder Schriftenreihe: Journal of Geophysical Research: Atmospheres
Jahrgang/Volume einer Zeitschrift: 126
(Heft-)Nummer: 17
Kollation: 27 Seiten
DOI: 10.26083/tuprints-00020979
URL / URN: https://tuprints.ulb.tu-darmstadt.de/20979
Zugehörige Links:
Herkunft: Zweitveröffentlichung DeepGreen
Kurzbeschreibung (Abstract):

Volcanic ash (VA) from explosive eruptions contributes to aerosol loadings in the atmosphere. Aside from the negative impact of VA on air quality and aviation, these particles can alter the optical and microphysical properties of clouds by triggering ice formation, thereby influencing precipitation and climate. Depending on the volcano and eruption style, VA displays a wide range of different physical, chemical, and mineralogical properties. Here, we present a unique data set on the ice nucleation activity of 15 VA samples obtained from different volcanoes worldwide. The ice nucleation activities of these samples were studied in the Aerosol Interaction and Dynamics in the Atmosphere (AIDA) cloud simulation chamber as well as with the Ice Nucleation Spectrometer of the Karlsruhe Institute of Technology (INSEKT). All VA particles nucleated ice in the immersion freezing mode from 263 to 238K with ice nucleation active site (INAS) densities ranging from ∼10⁵ to 10¹¹ m⁻², respectively. The variabilities observed among the VA samples, at any given temperature, range over 3.5 orders of magnitude. The ice‐nucleating abilities of VA samples correlate to varying degrees with their bulk pyroxene and plagioclase contents as a function of temperature. We combined our new data set with existing literature data to develop an improved ice nucleation parameterization for natural VA in the immersion freezing mode. This should be useful for modeling the impact of VA on clouds.

Freie Schlagworte: aerosol, chemical composition, cloud chamber, ice nucleation, mineralogy, mixed‐phase clouds, parameterization, volcanic ash
ID-Nummer: Artikel-ID: e2020JD033356
Status: Verlagsversion
URN: urn:nbn:de:tuda-tuprints-209791
Sachgruppe der Dewey Dezimalklassifikatin (DDC): 500 Naturwissenschaften und Mathematik > 550 Geowissenschaften
Fachbereich(e)/-gebiet(e): 11 Fachbereich Material- und Geowissenschaften
11 Fachbereich Material- und Geowissenschaften > Geowissenschaften
11 Fachbereich Material- und Geowissenschaften > Geowissenschaften > Fachgebiet Atmosphärisches Aerosol
Hinterlegungsdatum: 13 Feb 2024 13:32
Letzte Änderung: 14 Feb 2024 08:00
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