Aerosol Effect on the Cloud Phase of Low-Level Clouds Over the Arctic
Three years of nighttime Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation data was used in synergy with CloudSat measurements to quantify how strongly aerosol type and aerosol load affect the cloud phase in low-level clouds over the Arctic. Supercooled liquid layers were present in...
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ftnkunivathens:oai:lib.uoa.gr:uoadl:3069065 2024-02-11T10:00:48+01:00 Aerosol Effect on the Cloud Phase of Low-Level Clouds Over the Arctic Filioglou, M. Mielonen, T. Balis, D. Giannakaki, E. Arola, A. Kokkola, H. Komppula, M. Romakkaniemi, S. 2019-01-01 https://pergamos.lib.uoa.gr/uoa/dl/object/uoadl:3069065 Αγγλικά English eng uoadl:3069065 https://pergamos.lib.uoa.gr/uoa/dl/object/uoadl:3069065 scientific_publication_article Επιστημονική δημοσίευση - Άρθρο Περιοδικού Scientific publication - Journal Article 2019 ftnkunivathens 2024-01-18T19:12:50Z Three years of nighttime Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation data was used in synergy with CloudSat measurements to quantify how strongly aerosol type and aerosol load affect the cloud phase in low-level clouds over the Arctic. Supercooled liquid layers were present in the majority of observed low-level clouds (0.75 ≤ z ≤ 3.5 km) between −10 and −25 °C. Furthermore, based on the subset (6%) of data with high quality assurance for aerosol typing, ice formation is more common in the presence of dust or continental aerosols as opposed to marine or elevated smoke aerosols. With the first aerosol group, glaciated clouds were found at cloud top temperatures of 2 to 4 °C warmer than with the latter aerosol types. Further association of the aerosol concentration with the cloud phase showed that the aerosol concentration outweighs the aerosol type effect. Depending on the aerosol load, the temperature at which a cloud completely glaciates can vary by up to 6–10 °C. However, this behavior was most pronounced in stable atmospheric conditions and absent over open ocean with lower tropospheric stability values and probably less stratified clouds. Finally, more mixed-phase clouds were associated with high aerosol load, suggesting that mixed-phase clouds have an extended lifetime in the Arctic under high cloud condensation nuclei concentrations. This implies that in a pristine environment, with few or no local aerosol sources, and under the investigated conditions the amount of aerosol particles affects the cloud phase more than the aerosol type does. ©2019. American Geophysical Union. All Rights Reserved. Article in Journal/Newspaper Arctic Pergamos - Library and Information Center of National and Kapodistrian University of Athens Arctic |
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Open Polar |
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Pergamos - Library and Information Center of National and Kapodistrian University of Athens |
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ftnkunivathens |
language |
English |
description |
Three years of nighttime Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation data was used in synergy with CloudSat measurements to quantify how strongly aerosol type and aerosol load affect the cloud phase in low-level clouds over the Arctic. Supercooled liquid layers were present in the majority of observed low-level clouds (0.75 ≤ z ≤ 3.5 km) between −10 and −25 °C. Furthermore, based on the subset (6%) of data with high quality assurance for aerosol typing, ice formation is more common in the presence of dust or continental aerosols as opposed to marine or elevated smoke aerosols. With the first aerosol group, glaciated clouds were found at cloud top temperatures of 2 to 4 °C warmer than with the latter aerosol types. Further association of the aerosol concentration with the cloud phase showed that the aerosol concentration outweighs the aerosol type effect. Depending on the aerosol load, the temperature at which a cloud completely glaciates can vary by up to 6–10 °C. However, this behavior was most pronounced in stable atmospheric conditions and absent over open ocean with lower tropospheric stability values and probably less stratified clouds. Finally, more mixed-phase clouds were associated with high aerosol load, suggesting that mixed-phase clouds have an extended lifetime in the Arctic under high cloud condensation nuclei concentrations. This implies that in a pristine environment, with few or no local aerosol sources, and under the investigated conditions the amount of aerosol particles affects the cloud phase more than the aerosol type does. ©2019. American Geophysical Union. All Rights Reserved. |
format |
Article in Journal/Newspaper |
author |
Filioglou, M. Mielonen, T. Balis, D. Giannakaki, E. Arola, A. Kokkola, H. Komppula, M. Romakkaniemi, S. |
spellingShingle |
Filioglou, M. Mielonen, T. Balis, D. Giannakaki, E. Arola, A. Kokkola, H. Komppula, M. Romakkaniemi, S. Aerosol Effect on the Cloud Phase of Low-Level Clouds Over the Arctic |
author_facet |
Filioglou, M. Mielonen, T. Balis, D. Giannakaki, E. Arola, A. Kokkola, H. Komppula, M. Romakkaniemi, S. |
author_sort |
Filioglou, M. |
title |
Aerosol Effect on the Cloud Phase of Low-Level Clouds Over the Arctic |
title_short |
Aerosol Effect on the Cloud Phase of Low-Level Clouds Over the Arctic |
title_full |
Aerosol Effect on the Cloud Phase of Low-Level Clouds Over the Arctic |
title_fullStr |
Aerosol Effect on the Cloud Phase of Low-Level Clouds Over the Arctic |
title_full_unstemmed |
Aerosol Effect on the Cloud Phase of Low-Level Clouds Over the Arctic |
title_sort |
aerosol effect on the cloud phase of low-level clouds over the arctic |
publishDate |
2019 |
url |
https://pergamos.lib.uoa.gr/uoa/dl/object/uoadl:3069065 |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic |
genre_facet |
Arctic |
op_relation |
uoadl:3069065 https://pergamos.lib.uoa.gr/uoa/dl/object/uoadl:3069065 |
_version_ |
1790596519086260224 |