The importance of Aitken mode aerosol particles for cloud sustenance in the summertime high Arctic-A simulation study supported by observational data

The potential importance of Aitken mode particles (diameters 25 80 nm) for stratiform mixed-phase clouds in the summertime high Arctic (80 N) has been investigated using two large-eddy simulation models. We find that, in both models, Aitken mode particles significantly affect the simulated microphys...

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Main Authors: Bulatovic, I, Igel, AL, Leck, C, Heintzenberg, J, Riipinen, I, Ekman, AML
Format: Article in Journal/Newspaper
Language:unknown
Published: eScholarship, University of California 2021
Subjects:
Online Access:https://escholarship.org/uc/item/27259683
id ftcdlib:oai:escholarship.org/ark:/13030/qt27259683
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spelling ftcdlib:oai:escholarship.org/ark:/13030/qt27259683 2023-05-15T14:48:15+02:00 The importance of Aitken mode aerosol particles for cloud sustenance in the summertime high Arctic-A simulation study supported by observational data Bulatovic, I Igel, AL Leck, C Heintzenberg, J Riipinen, I Ekman, AML 3871 - 3897 2021-03-15 https://escholarship.org/uc/item/27259683 unknown eScholarship, University of California qt27259683 https://escholarship.org/uc/item/27259683 public Atmospheric Chemistry and Physics, vol 21, iss 5 Astronomical and Space Sciences Atmospheric Sciences Meteorology & Atmospheric Sciences article 2021 ftcdlib 2021-04-16T07:11:30Z The potential importance of Aitken mode particles (diameters 25 80 nm) for stratiform mixed-phase clouds in the summertime high Arctic (80 N) has been investigated using two large-eddy simulation models. We find that, in both models, Aitken mode particles significantly affect the simulated microphysical and radiative properties of the cloud and can help sustain the cloud when accumulation mode concentrations are low (10 20 cm3), even when the particles have low hygroscopicity (hygroscopicity parameter-D 0:1). However, the influence of the Aitken mode decreases if the overall liquid water content of the cloud is low, either due to a higher ice fraction or due to low radiative cooling rates. An analysis of the simulated supersaturation (ss) statistics shows that the ss frequently reaches 0.5% and sometimes even exceeds 1 %, which confirms that Aitken mode particles can be activated. The modelling results are in qualitative agreement with observations of the Hoppel minimum obtained from four different expeditions in the high Arctic. Our findings highlight the importance of better understanding Aitken mode particle formation, chemical properties and emissions, particularly in clean environments such as the high Arctic. Article in Journal/Newspaper Arctic University of California: eScholarship Arctic Aitken ENVELOPE(-44.516,-44.516,-60.733,-60.733)
institution Open Polar
collection University of California: eScholarship
op_collection_id ftcdlib
language unknown
topic Astronomical and Space Sciences
Atmospheric Sciences
Meteorology & Atmospheric Sciences
spellingShingle Astronomical and Space Sciences
Atmospheric Sciences
Meteorology & Atmospheric Sciences
Bulatovic, I
Igel, AL
Leck, C
Heintzenberg, J
Riipinen, I
Ekman, AML
The importance of Aitken mode aerosol particles for cloud sustenance in the summertime high Arctic-A simulation study supported by observational data
topic_facet Astronomical and Space Sciences
Atmospheric Sciences
Meteorology & Atmospheric Sciences
description The potential importance of Aitken mode particles (diameters 25 80 nm) for stratiform mixed-phase clouds in the summertime high Arctic (80 N) has been investigated using two large-eddy simulation models. We find that, in both models, Aitken mode particles significantly affect the simulated microphysical and radiative properties of the cloud and can help sustain the cloud when accumulation mode concentrations are low (10 20 cm3), even when the particles have low hygroscopicity (hygroscopicity parameter-D 0:1). However, the influence of the Aitken mode decreases if the overall liquid water content of the cloud is low, either due to a higher ice fraction or due to low radiative cooling rates. An analysis of the simulated supersaturation (ss) statistics shows that the ss frequently reaches 0.5% and sometimes even exceeds 1 %, which confirms that Aitken mode particles can be activated. The modelling results are in qualitative agreement with observations of the Hoppel minimum obtained from four different expeditions in the high Arctic. Our findings highlight the importance of better understanding Aitken mode particle formation, chemical properties and emissions, particularly in clean environments such as the high Arctic.
format Article in Journal/Newspaper
author Bulatovic, I
Igel, AL
Leck, C
Heintzenberg, J
Riipinen, I
Ekman, AML
author_facet Bulatovic, I
Igel, AL
Leck, C
Heintzenberg, J
Riipinen, I
Ekman, AML
author_sort Bulatovic, I
title The importance of Aitken mode aerosol particles for cloud sustenance in the summertime high Arctic-A simulation study supported by observational data
title_short The importance of Aitken mode aerosol particles for cloud sustenance in the summertime high Arctic-A simulation study supported by observational data
title_full The importance of Aitken mode aerosol particles for cloud sustenance in the summertime high Arctic-A simulation study supported by observational data
title_fullStr The importance of Aitken mode aerosol particles for cloud sustenance in the summertime high Arctic-A simulation study supported by observational data
title_full_unstemmed The importance of Aitken mode aerosol particles for cloud sustenance in the summertime high Arctic-A simulation study supported by observational data
title_sort importance of aitken mode aerosol particles for cloud sustenance in the summertime high arctic-a simulation study supported by observational data
publisher eScholarship, University of California
publishDate 2021
url https://escholarship.org/uc/item/27259683
op_coverage 3871 - 3897
long_lat ENVELOPE(-44.516,-44.516,-60.733,-60.733)
geographic Arctic
Aitken
geographic_facet Arctic
Aitken
genre Arctic
genre_facet Arctic
op_source Atmospheric Chemistry and Physics, vol 21, iss 5
op_relation qt27259683
https://escholarship.org/uc/item/27259683
op_rights public
_version_ 1766319342573584384