Measurement report: In-situ vertical profiles of below-cloud aerosol over the central Greenland Ice Sheet

Surface radiative cooling in polar regions can generate persistent stability in the atmospheric boundary layer. Stable layers below clouds can decouple the cloud layer from the near-surface environment. Under these conditions, surface aerosol measurements are not necessarily representative of the ne...

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Main Authors: Guy, Heather, Martin, Andrew S., Olson, Erik, Brooks, Ian M., Neely III, Ryan R.
Format: Text
Language:English
Published: 2024
Subjects:
Online Access:https://doi.org/10.5194/egusphere-2024-733
https://egusphere.copernicus.org/preprints/2024/egusphere-2024-733/
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spelling ftcopernicus:oai:publications.copernicus.org:egusphere118739 2024-09-15T18:09:01+00:00 Measurement report: In-situ vertical profiles of below-cloud aerosol over the central Greenland Ice Sheet Guy, Heather Martin, Andrew S. Olson, Erik Brooks, Ian M. Neely III, Ryan R. 2024-03-19 application/pdf https://doi.org/10.5194/egusphere-2024-733 https://egusphere.copernicus.org/preprints/2024/egusphere-2024-733/ eng eng doi:10.5194/egusphere-2024-733 https://egusphere.copernicus.org/preprints/2024/egusphere-2024-733/ eISSN: Text 2024 ftcopernicus https://doi.org/10.5194/egusphere-2024-733 2024-08-28T05:24:15Z Surface radiative cooling in polar regions can generate persistent stability in the atmospheric boundary layer. Stable layers below clouds can decouple the cloud layer from the near-surface environment. Under these conditions, surface aerosol measurements are not necessarily representative of the near-cloud or intra-cloud aerosol populations. To better understand the variability in the vertical structure of aerosol properties over the central Greenland Ice Sheet, in-situ measurements of aerosol particle size distributions up to cloud base were made at Summit Station in July and August 2023. These measurements identified distinct vertical aerosol layers between the surface and cloud base associated thermodynamic decoupling layers. Such decoupling layers occur 49 % of the time during the summer in central Greenland, suggesting that surface aerosol measurements are insufficient to describe the cloud-relevant aerosol population half of the time. Experience during this first measurement season demonstrated the ability of a tethered balloon platform to operate effectively under icing conditions and at low surface pressure (< 680 hPa). The results presented here illustrate the value of vertically resolved in-situ measurements of aerosol properties to develop a nuanced understanding of the aerosol effects on cloud properties in polar regions. Text Greenland Ice Sheet Copernicus Publications: E-Journals
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description Surface radiative cooling in polar regions can generate persistent stability in the atmospheric boundary layer. Stable layers below clouds can decouple the cloud layer from the near-surface environment. Under these conditions, surface aerosol measurements are not necessarily representative of the near-cloud or intra-cloud aerosol populations. To better understand the variability in the vertical structure of aerosol properties over the central Greenland Ice Sheet, in-situ measurements of aerosol particle size distributions up to cloud base were made at Summit Station in July and August 2023. These measurements identified distinct vertical aerosol layers between the surface and cloud base associated thermodynamic decoupling layers. Such decoupling layers occur 49 % of the time during the summer in central Greenland, suggesting that surface aerosol measurements are insufficient to describe the cloud-relevant aerosol population half of the time. Experience during this first measurement season demonstrated the ability of a tethered balloon platform to operate effectively under icing conditions and at low surface pressure (< 680 hPa). The results presented here illustrate the value of vertically resolved in-situ measurements of aerosol properties to develop a nuanced understanding of the aerosol effects on cloud properties in polar regions.
format Text
author Guy, Heather
Martin, Andrew S.
Olson, Erik
Brooks, Ian M.
Neely III, Ryan R.
spellingShingle Guy, Heather
Martin, Andrew S.
Olson, Erik
Brooks, Ian M.
Neely III, Ryan R.
Measurement report: In-situ vertical profiles of below-cloud aerosol over the central Greenland Ice Sheet
author_facet Guy, Heather
Martin, Andrew S.
Olson, Erik
Brooks, Ian M.
Neely III, Ryan R.
author_sort Guy, Heather
title Measurement report: In-situ vertical profiles of below-cloud aerosol over the central Greenland Ice Sheet
title_short Measurement report: In-situ vertical profiles of below-cloud aerosol over the central Greenland Ice Sheet
title_full Measurement report: In-situ vertical profiles of below-cloud aerosol over the central Greenland Ice Sheet
title_fullStr Measurement report: In-situ vertical profiles of below-cloud aerosol over the central Greenland Ice Sheet
title_full_unstemmed Measurement report: In-situ vertical profiles of below-cloud aerosol over the central Greenland Ice Sheet
title_sort measurement report: in-situ vertical profiles of below-cloud aerosol over the central greenland ice sheet
publishDate 2024
url https://doi.org/10.5194/egusphere-2024-733
https://egusphere.copernicus.org/preprints/2024/egusphere-2024-733/
genre Greenland
Ice Sheet
genre_facet Greenland
Ice Sheet
op_source eISSN:
op_relation doi:10.5194/egusphere-2024-733
https://egusphere.copernicus.org/preprints/2024/egusphere-2024-733/
op_doi https://doi.org/10.5194/egusphere-2024-733
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