Experimental investigation of homogeneous freezing of sulphuric acid particles in the aerosol chamber AIDA

The homogeneous freezing of supercooled H<sub>2</sub>SO<sub>4</sub>/H<sub>2</sub>O solution droplets was investigated in the aerosol chamber AIDA (Aerosol Interactions and Dynamics in the Atmosphere) of Forschungszentrum Karlsruhe. 24 freezing experiments were...

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Main Authors: O. Möhler, O. Stetzer, S. Schaefers, C. Linke, M. Schnaiter, R. Tiede, H. Saathoff, M. Krämer, A. Mangold, P. Budz, P. Zink, J. Schreiner, K. Mauersberger, W. Haag, B. Kärcher, U. Schurath
Format: Article
Language:English
Published: Copernicus Publications 2003-01-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/3/211/2003/acp-3-211-2003.pdf
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spelling doaj-41af082c4b3645608555e0033aa8a3302020-11-24T21:12:29ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242003-01-0131211223Experimental investigation of homogeneous freezing of sulphuric acid particles in the aerosol chamber AIDAO. MöhlerO. StetzerS. SchaefersC. LinkeM. SchnaiterR. TiedeH. SaathoffM. KrämerA. MangoldP. BudzP. ZinkJ. SchreinerK. MauersbergerW. HaagB. KärcherU. SchurathThe homogeneous freezing of supercooled H<sub>2</sub>SO<sub>4</sub>/H<sub>2</sub>O solution droplets was investigated in the aerosol chamber AIDA (Aerosol Interactions and Dynamics in the Atmosphere) of Forschungszentrum Karlsruhe. 24 freezing experiments were performed at temperatures between 189 and 235 K with aerosol particles in the diameter range 0.05 to 1 µm. Individual experiments started at homogeneous temperatures and ice saturation ratios between 0.9 and 0.95. Cloud cooling rates up to -2.8 K min<sup>-1</sup> were simulated dynamically in the chamber by expansion cooling using a mechanical pump. Depending on the cooling rate and starting temperature, freezing threshold relative humidities were exceeded after expansion time periods between about 1 and 10 min. The onset of ice formation was measured with three independent methods showing good agreement among each other. Ice saturation ratios measured at the onset of ice formation increased from about 1.4 at 231 K&nbsp; to about 1.75 at 189 K. The experimental data set including thermodynamic parameters as well as physical and chemical aerosol analysis provides a good basis for microphysical model applications.http://www.atmos-chem-phys.net/3/211/2003/acp-3-211-2003.pdf
collection DOAJ
language English
format Article
sources DOAJ
author O. Möhler
O. Stetzer
S. Schaefers
C. Linke
M. Schnaiter
R. Tiede
H. Saathoff
M. Krämer
A. Mangold
P. Budz
P. Zink
J. Schreiner
K. Mauersberger
W. Haag
B. Kärcher
U. Schurath
spellingShingle O. Möhler
O. Stetzer
S. Schaefers
C. Linke
M. Schnaiter
R. Tiede
H. Saathoff
M. Krämer
A. Mangold
P. Budz
P. Zink
J. Schreiner
K. Mauersberger
W. Haag
B. Kärcher
U. Schurath
Experimental investigation of homogeneous freezing of sulphuric acid particles in the aerosol chamber AIDA
Atmospheric Chemistry and Physics
author_facet O. Möhler
O. Stetzer
S. Schaefers
C. Linke
M. Schnaiter
R. Tiede
H. Saathoff
M. Krämer
A. Mangold
P. Budz
P. Zink
J. Schreiner
K. Mauersberger
W. Haag
B. Kärcher
U. Schurath
author_sort O. Möhler
title Experimental investigation of homogeneous freezing of sulphuric acid particles in the aerosol chamber AIDA
title_short Experimental investigation of homogeneous freezing of sulphuric acid particles in the aerosol chamber AIDA
title_full Experimental investigation of homogeneous freezing of sulphuric acid particles in the aerosol chamber AIDA
title_fullStr Experimental investigation of homogeneous freezing of sulphuric acid particles in the aerosol chamber AIDA
title_full_unstemmed Experimental investigation of homogeneous freezing of sulphuric acid particles in the aerosol chamber AIDA
title_sort experimental investigation of homogeneous freezing of sulphuric acid particles in the aerosol chamber aida
publisher Copernicus Publications
series Atmospheric Chemistry and Physics
issn 1680-7316
1680-7324
publishDate 2003-01-01
description The homogeneous freezing of supercooled H<sub>2</sub>SO<sub>4</sub>/H<sub>2</sub>O solution droplets was investigated in the aerosol chamber AIDA (Aerosol Interactions and Dynamics in the Atmosphere) of Forschungszentrum Karlsruhe. 24 freezing experiments were performed at temperatures between 189 and 235 K with aerosol particles in the diameter range 0.05 to 1 µm. Individual experiments started at homogeneous temperatures and ice saturation ratios between 0.9 and 0.95. Cloud cooling rates up to -2.8 K min<sup>-1</sup> were simulated dynamically in the chamber by expansion cooling using a mechanical pump. Depending on the cooling rate and starting temperature, freezing threshold relative humidities were exceeded after expansion time periods between about 1 and 10 min. The onset of ice formation was measured with three independent methods showing good agreement among each other. Ice saturation ratios measured at the onset of ice formation increased from about 1.4 at 231 K&nbsp; to about 1.75 at 189 K. The experimental data set including thermodynamic parameters as well as physical and chemical aerosol analysis provides a good basis for microphysical model applications.
url http://www.atmos-chem-phys.net/3/211/2003/acp-3-211-2003.pdf
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