Wintertime Airborne Measurements of Ice Nucleating Particles in the High Arctic: A Hint to a Marine, Biogenic Source for Ice Nucleating Particles

Ice nucleating particles (INPs) affect the radiative properties of cold clouds. Knowledge concerning their concentration above ground level and their potential sources is scarce. Here we present the first highly temperature resolved ice nucleation spectra of airborne samples from an aircraft campaig...

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Published in:Environmental Research Letters
Main Authors: Hartmann, M., Adachi, K., Eppers, O., Haas, C., Herber, A., Holzinger, R., Hünerbein, A., Jäkel, E., Jentzsch, C., van Pinxteren, M., Wex, H., Willmes, S., Stratmann, F.
Format: Article in Journal/Newspaper
Language:English
Published: Hoboken, NJ [u.a.] : Wiley 2020
Subjects:
Online Access:https://oa.tib.eu/renate/handle/123456789/7236
https://doi.org/10.34657/6283
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author Hartmann, M.
Adachi, K.
Eppers, O.
Haas, C.
Herber, A.
Holzinger, R.
Hünerbein, A.
Jäkel, E.
Jentzsch, C.
van Pinxteren, M.
Wex, H.
Willmes, S.
Stratmann, F.
author_facet Hartmann, M.
Adachi, K.
Eppers, O.
Haas, C.
Herber, A.
Holzinger, R.
Hünerbein, A.
Jäkel, E.
Jentzsch, C.
van Pinxteren, M.
Wex, H.
Willmes, S.
Stratmann, F.
author_sort Hartmann, M.
collection LeibnizOpen (The Leibniz Association)
container_issue 9
container_start_page 094042
container_title Environmental Research Letters
container_volume 18
description Ice nucleating particles (INPs) affect the radiative properties of cold clouds. Knowledge concerning their concentration above ground level and their potential sources is scarce. Here we present the first highly temperature resolved ice nucleation spectra of airborne samples from an aircraft campaign during late winter in 2018. Most INP spectra featured low concentration levels (<3 · 10−4 L−1 at −15°C). However, we also found INP concentrations of up to 1.8·10−2 L−1 at −15°C and freezing onsets as high as −7.5°C for samples mainly from the marine boundary layer. Shape and onset temperature of the ice nucleation spectra of those samples as well as heat sensitivity hint at biogenic INP. Colocated measurements additionally indicate a local marine influence rather than long-range transport. Our results suggest that even in late winter above 80°N a local marine source for biogenic INP, which can efficiently nucleate ice at high temperatures, is present. ©2020. The Authors. publishedVersion
format Article in Journal/Newspaper
genre Arctic
genre_facet Arctic
geographic Arctic
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op_doi https://doi.org/10.34657/6283
op_rights CC BY 4.0 Unported
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op_source Geophysical Research Letters 47 (2020), Nr. 13
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spelling ftleibnizopen:oai:oai.leibnizopen.de:ttJDfYoBNQPDO7WI6XJV 2025-01-16T20:20:44+00:00 Wintertime Airborne Measurements of Ice Nucleating Particles in the High Arctic: A Hint to a Marine, Biogenic Source for Ice Nucleating Particles Hartmann, M. Adachi, K. Eppers, O. Haas, C. Herber, A. Holzinger, R. Hünerbein, A. Jäkel, E. Jentzsch, C. van Pinxteren, M. Wex, H. Willmes, S. Stratmann, F. 2020 application/pdf https://oa.tib.eu/renate/handle/123456789/7236 https://doi.org/10.34657/6283 eng eng Hoboken, NJ [u.a.] : Wiley CC BY 4.0 Unported https://creativecommons.org/licenses/by/4.0/ Geophysical Research Letters 47 (2020), Nr. 13 aerosol-cloud interactions Arctic Arctic aerosol ice nucleating particles 550 article Text 2020 ftleibnizopen https://doi.org/10.34657/6283 2023-09-10T23:17:45Z Ice nucleating particles (INPs) affect the radiative properties of cold clouds. Knowledge concerning their concentration above ground level and their potential sources is scarce. Here we present the first highly temperature resolved ice nucleation spectra of airborne samples from an aircraft campaign during late winter in 2018. Most INP spectra featured low concentration levels (<3 · 10−4 L−1 at −15°C). However, we also found INP concentrations of up to 1.8·10−2 L−1 at −15°C and freezing onsets as high as −7.5°C for samples mainly from the marine boundary layer. Shape and onset temperature of the ice nucleation spectra of those samples as well as heat sensitivity hint at biogenic INP. Colocated measurements additionally indicate a local marine influence rather than long-range transport. Our results suggest that even in late winter above 80°N a local marine source for biogenic INP, which can efficiently nucleate ice at high temperatures, is present. ©2020. The Authors. publishedVersion Article in Journal/Newspaper Arctic LeibnizOpen (The Leibniz Association) Arctic Environmental Research Letters 18 9 094042
spellingShingle aerosol-cloud interactions
Arctic
Arctic aerosol
ice nucleating particles
550
Hartmann, M.
Adachi, K.
Eppers, O.
Haas, C.
Herber, A.
Holzinger, R.
Hünerbein, A.
Jäkel, E.
Jentzsch, C.
van Pinxteren, M.
Wex, H.
Willmes, S.
Stratmann, F.
Wintertime Airborne Measurements of Ice Nucleating Particles in the High Arctic: A Hint to a Marine, Biogenic Source for Ice Nucleating Particles
title Wintertime Airborne Measurements of Ice Nucleating Particles in the High Arctic: A Hint to a Marine, Biogenic Source for Ice Nucleating Particles
title_full Wintertime Airborne Measurements of Ice Nucleating Particles in the High Arctic: A Hint to a Marine, Biogenic Source for Ice Nucleating Particles
title_fullStr Wintertime Airborne Measurements of Ice Nucleating Particles in the High Arctic: A Hint to a Marine, Biogenic Source for Ice Nucleating Particles
title_full_unstemmed Wintertime Airborne Measurements of Ice Nucleating Particles in the High Arctic: A Hint to a Marine, Biogenic Source for Ice Nucleating Particles
title_short Wintertime Airborne Measurements of Ice Nucleating Particles in the High Arctic: A Hint to a Marine, Biogenic Source for Ice Nucleating Particles
title_sort wintertime airborne measurements of ice nucleating particles in the high arctic: a hint to a marine, biogenic source for ice nucleating particles
topic aerosol-cloud interactions
Arctic
Arctic aerosol
ice nucleating particles
550
topic_facet aerosol-cloud interactions
Arctic
Arctic aerosol
ice nucleating particles
550
url https://oa.tib.eu/renate/handle/123456789/7236
https://doi.org/10.34657/6283