Annual cycle of aerosol properties over the central Arctic during MOSAiC 2019–2020 – light-extinction, CCN, and INP levels from the boundary layer to the tropopause
The MOSAiC (Multidisciplinary drifting Observatory for the Study of Arctic Climate) expedition was the largest Arctic field campaign ever conducted. MOSAiC offered the unique opportunity to monitor and characterize aerosols and clouds with high vertical resolution up to 30 km height at latitudes fro...
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2023
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Online Access: | https://doi.org/10.5194/acp-23-12821-2023 https://doaj.org/article/b0817dddeb4144e38a913c911681ba5c |
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ftdoajarticles:oai:doaj.org/article:b0817dddeb4144e38a913c911681ba5c 2023-11-12T04:11:39+01:00 Annual cycle of aerosol properties over the central Arctic during MOSAiC 2019–2020 – light-extinction, CCN, and INP levels from the boundary layer to the tropopause A. Ansmann K. Ohneiser R. Engelmann M. Radenz H. Griesche J. Hofer D. Althausen J. M. Creamean M. C. Boyer D. A. Knopf S. Dahlke M. Maturilli H. Gebauer J. Bühl C. Jimenez P. Seifert U. Wandinger 2023-10-01T00:00:00Z https://doi.org/10.5194/acp-23-12821-2023 https://doaj.org/article/b0817dddeb4144e38a913c911681ba5c EN eng Copernicus Publications https://acp.copernicus.org/articles/23/12821/2023/acp-23-12821-2023.pdf https://doaj.org/toc/1680-7316 https://doaj.org/toc/1680-7324 doi:10.5194/acp-23-12821-2023 1680-7316 1680-7324 https://doaj.org/article/b0817dddeb4144e38a913c911681ba5c Atmospheric Chemistry and Physics, Vol 23, Pp 12821-12849 (2023) Physics QC1-999 Chemistry QD1-999 article 2023 ftdoajarticles https://doi.org/10.5194/acp-23-12821-2023 2023-10-15T00:37:04Z The MOSAiC (Multidisciplinary drifting Observatory for the Study of Arctic Climate) expedition was the largest Arctic field campaign ever conducted. MOSAiC offered the unique opportunity to monitor and characterize aerosols and clouds with high vertical resolution up to 30 km height at latitudes from 80 to 90 ∘ N over an entire year (October 2019 to September 2020). Without a clear knowledge of the complex aerosol layering, vertical structures, and dominant aerosol types and their impact on cloud formation, a full understanding of the meteorological processes in the Arctic, and thus advanced climate change research, is impossible. Widespread ground-based in situ observations in the Arctic are insufficient to provide these required aerosol and cloud data. In this article, a summary of our MOSAiC observations of tropospheric aerosol profiles with a state-of-the-art multiwavelength polarization Raman lidar aboard the icebreaker Polarstern is presented. Particle optical properties, i.e., light-extinction profiles and aerosol optical thickness (AOT), and estimates of cloud-relevant aerosol properties such as the number concentration of cloud condensation nuclei (CCN) and ice-nucleating particles (INPs) are discussed, separately for the lowest part of the troposphere (atmospheric boundary layer, ABL), within the lower free troposphere (around 2000 m height), and at the cirrus level close to the tropopause. In situ observations of the particle number concentration and INPs aboard Polarstern are included in the study. A strong decrease in the aerosol amount with height in winter and moderate vertical variations in summer were observed in terms of the particle extinction coefficient. The 532 nm light-extinction values dropped from >50 Mm −1 close to the surface to <5 Mm −1 at 4–6 km height in the winter months. Lofted, aged wildfire smoke layers caused a re-increase in the aerosol concentration towards the tropopause. In summer (June to August 2020), much lower particle extinction coefficients, frequently as low as ... Article in Journal/Newspaper Arctic Climate change Directory of Open Access Journals: DOAJ Articles Arctic Atmospheric Chemistry and Physics 23 19 12821 12849 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Physics QC1-999 Chemistry QD1-999 |
spellingShingle |
Physics QC1-999 Chemistry QD1-999 A. Ansmann K. Ohneiser R. Engelmann M. Radenz H. Griesche J. Hofer D. Althausen J. M. Creamean M. C. Boyer D. A. Knopf S. Dahlke M. Maturilli H. Gebauer J. Bühl C. Jimenez P. Seifert U. Wandinger Annual cycle of aerosol properties over the central Arctic during MOSAiC 2019–2020 – light-extinction, CCN, and INP levels from the boundary layer to the tropopause |
topic_facet |
Physics QC1-999 Chemistry QD1-999 |
description |
The MOSAiC (Multidisciplinary drifting Observatory for the Study of Arctic Climate) expedition was the largest Arctic field campaign ever conducted. MOSAiC offered the unique opportunity to monitor and characterize aerosols and clouds with high vertical resolution up to 30 km height at latitudes from 80 to 90 ∘ N over an entire year (October 2019 to September 2020). Without a clear knowledge of the complex aerosol layering, vertical structures, and dominant aerosol types and their impact on cloud formation, a full understanding of the meteorological processes in the Arctic, and thus advanced climate change research, is impossible. Widespread ground-based in situ observations in the Arctic are insufficient to provide these required aerosol and cloud data. In this article, a summary of our MOSAiC observations of tropospheric aerosol profiles with a state-of-the-art multiwavelength polarization Raman lidar aboard the icebreaker Polarstern is presented. Particle optical properties, i.e., light-extinction profiles and aerosol optical thickness (AOT), and estimates of cloud-relevant aerosol properties such as the number concentration of cloud condensation nuclei (CCN) and ice-nucleating particles (INPs) are discussed, separately for the lowest part of the troposphere (atmospheric boundary layer, ABL), within the lower free troposphere (around 2000 m height), and at the cirrus level close to the tropopause. In situ observations of the particle number concentration and INPs aboard Polarstern are included in the study. A strong decrease in the aerosol amount with height in winter and moderate vertical variations in summer were observed in terms of the particle extinction coefficient. The 532 nm light-extinction values dropped from >50 Mm −1 close to the surface to <5 Mm −1 at 4–6 km height in the winter months. Lofted, aged wildfire smoke layers caused a re-increase in the aerosol concentration towards the tropopause. In summer (June to August 2020), much lower particle extinction coefficients, frequently as low as ... |
format |
Article in Journal/Newspaper |
author |
A. Ansmann K. Ohneiser R. Engelmann M. Radenz H. Griesche J. Hofer D. Althausen J. M. Creamean M. C. Boyer D. A. Knopf S. Dahlke M. Maturilli H. Gebauer J. Bühl C. Jimenez P. Seifert U. Wandinger |
author_facet |
A. Ansmann K. Ohneiser R. Engelmann M. Radenz H. Griesche J. Hofer D. Althausen J. M. Creamean M. C. Boyer D. A. Knopf S. Dahlke M. Maturilli H. Gebauer J. Bühl C. Jimenez P. Seifert U. Wandinger |
author_sort |
A. Ansmann |
title |
Annual cycle of aerosol properties over the central Arctic during MOSAiC 2019–2020 – light-extinction, CCN, and INP levels from the boundary layer to the tropopause |
title_short |
Annual cycle of aerosol properties over the central Arctic during MOSAiC 2019–2020 – light-extinction, CCN, and INP levels from the boundary layer to the tropopause |
title_full |
Annual cycle of aerosol properties over the central Arctic during MOSAiC 2019–2020 – light-extinction, CCN, and INP levels from the boundary layer to the tropopause |
title_fullStr |
Annual cycle of aerosol properties over the central Arctic during MOSAiC 2019–2020 – light-extinction, CCN, and INP levels from the boundary layer to the tropopause |
title_full_unstemmed |
Annual cycle of aerosol properties over the central Arctic during MOSAiC 2019–2020 – light-extinction, CCN, and INP levels from the boundary layer to the tropopause |
title_sort |
annual cycle of aerosol properties over the central arctic during mosaic 2019–2020 – light-extinction, ccn, and inp levels from the boundary layer to the tropopause |
publisher |
Copernicus Publications |
publishDate |
2023 |
url |
https://doi.org/10.5194/acp-23-12821-2023 https://doaj.org/article/b0817dddeb4144e38a913c911681ba5c |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic Climate change |
genre_facet |
Arctic Climate change |
op_source |
Atmospheric Chemistry and Physics, Vol 23, Pp 12821-12849 (2023) |
op_relation |
https://acp.copernicus.org/articles/23/12821/2023/acp-23-12821-2023.pdf https://doaj.org/toc/1680-7316 https://doaj.org/toc/1680-7324 doi:10.5194/acp-23-12821-2023 1680-7316 1680-7324 https://doaj.org/article/b0817dddeb4144e38a913c911681ba5c |
op_doi |
https://doi.org/10.5194/acp-23-12821-2023 |
container_title |
Atmospheric Chemistry and Physics |
container_volume |
23 |
container_issue |
19 |
container_start_page |
12821 |
op_container_end_page |
12849 |
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