Environmental effects on aerosol–cloud interaction in non-precipitating marine boundary layer (MBL) clouds over the eastern North Atlantic
Over the eastern North Atlantic (ENA) ocean, a total of 20 non-precipitating single-layer marine boundary layer (MBL) stratus and stratocumulus cloud cases are selected to investigate the impacts of the environmental variables on the aerosol–cloud interaction ( ACI r ) using the ground-based measure...
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ftcopernicus:oai:publications.copernicus.org:acp94536 2023-05-15T17:32:58+02:00 Environmental effects on aerosol–cloud interaction in non-precipitating marine boundary layer (MBL) clouds over the eastern North Atlantic Zheng, Xiaojian Xi, Baike Dong, Xiquan Wu, Peng Logan, Timothy Wang, Yuan 2022-01-10 application/pdf https://doi.org/10.5194/acp-22-335-2022 https://acp.copernicus.org/articles/22/335/2022/ eng eng doi:10.5194/acp-22-335-2022 https://acp.copernicus.org/articles/22/335/2022/ eISSN: 1680-7324 Text 2022 ftcopernicus https://doi.org/10.5194/acp-22-335-2022 2022-01-17T17:22:18Z Over the eastern North Atlantic (ENA) ocean, a total of 20 non-precipitating single-layer marine boundary layer (MBL) stratus and stratocumulus cloud cases are selected to investigate the impacts of the environmental variables on the aerosol–cloud interaction ( ACI r ) using the ground-based measurements from the Department of Energy Atmospheric Radiation Measurement (ARM) facility at the ENA site during 2016–2018. The ACI r represents the relative change in cloud droplet effective radius r e with respect to the relative change in cloud condensation nuclei (CCN) number concentration at 0.2 % supersaturation ( N CCN,0.2 % ) in the stratified water vapor environment. The ACI r values vary from − 0.01 to 0.22 with increasing sub-cloud boundary layer precipitable water vapor ( PWV BL ) conditions, indicating that r e is more sensitive to the CCN loading under sufficient water vapor supply, owing to the combined effect of enhanced condensational growth and coalescence processes associated with higher N c and PWV BL . The principal component analysis shows that the most pronounced pattern during the selected cases is the co-variations in the MBL conditions characterized by the vertical component of turbulence kinetic energy ( TKE w ), the decoupling index ( D i ), and PWV BL . The environmental effects on ACI r emerge after the data are stratified into different TKE w regimes. The ACI r values, under both lower and higher PWV BL conditions, more than double from the low- TKE w to high- TKE w regime. This can be explained by the fact that stronger boundary layer turbulence maintains a well-mixed MBL, strengthening the connection between cloud microphysical properties and the below-cloud CCN and moisture sources. With sufficient water vapor and low CCN loading, the active coalescence process broadens the cloud droplet size spectra and consequently results in an enlargement of r e . The enhanced activation of CCN and the cloud droplet condensational growth induced by the higher below-cloud CCN loading can effectively decrease r e , which jointly presents as the increased ACI r . This study examines the importance of environmental effects on the ACI r assessments and provides observational constraints to future model evaluations of aerosol–cloud interactions. Text North Atlantic Copernicus Publications: E-Journals Atmospheric Chemistry and Physics 22 1 335 354 |
institution |
Open Polar |
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Copernicus Publications: E-Journals |
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ftcopernicus |
language |
English |
description |
Over the eastern North Atlantic (ENA) ocean, a total of 20 non-precipitating single-layer marine boundary layer (MBL) stratus and stratocumulus cloud cases are selected to investigate the impacts of the environmental variables on the aerosol–cloud interaction ( ACI r ) using the ground-based measurements from the Department of Energy Atmospheric Radiation Measurement (ARM) facility at the ENA site during 2016–2018. The ACI r represents the relative change in cloud droplet effective radius r e with respect to the relative change in cloud condensation nuclei (CCN) number concentration at 0.2 % supersaturation ( N CCN,0.2 % ) in the stratified water vapor environment. The ACI r values vary from − 0.01 to 0.22 with increasing sub-cloud boundary layer precipitable water vapor ( PWV BL ) conditions, indicating that r e is more sensitive to the CCN loading under sufficient water vapor supply, owing to the combined effect of enhanced condensational growth and coalescence processes associated with higher N c and PWV BL . The principal component analysis shows that the most pronounced pattern during the selected cases is the co-variations in the MBL conditions characterized by the vertical component of turbulence kinetic energy ( TKE w ), the decoupling index ( D i ), and PWV BL . The environmental effects on ACI r emerge after the data are stratified into different TKE w regimes. The ACI r values, under both lower and higher PWV BL conditions, more than double from the low- TKE w to high- TKE w regime. This can be explained by the fact that stronger boundary layer turbulence maintains a well-mixed MBL, strengthening the connection between cloud microphysical properties and the below-cloud CCN and moisture sources. With sufficient water vapor and low CCN loading, the active coalescence process broadens the cloud droplet size spectra and consequently results in an enlargement of r e . The enhanced activation of CCN and the cloud droplet condensational growth induced by the higher below-cloud CCN loading can effectively decrease r e , which jointly presents as the increased ACI r . This study examines the importance of environmental effects on the ACI r assessments and provides observational constraints to future model evaluations of aerosol–cloud interactions. |
format |
Text |
author |
Zheng, Xiaojian Xi, Baike Dong, Xiquan Wu, Peng Logan, Timothy Wang, Yuan |
spellingShingle |
Zheng, Xiaojian Xi, Baike Dong, Xiquan Wu, Peng Logan, Timothy Wang, Yuan Environmental effects on aerosol–cloud interaction in non-precipitating marine boundary layer (MBL) clouds over the eastern North Atlantic |
author_facet |
Zheng, Xiaojian Xi, Baike Dong, Xiquan Wu, Peng Logan, Timothy Wang, Yuan |
author_sort |
Zheng, Xiaojian |
title |
Environmental effects on aerosol–cloud interaction in non-precipitating marine boundary layer (MBL) clouds over the eastern North Atlantic |
title_short |
Environmental effects on aerosol–cloud interaction in non-precipitating marine boundary layer (MBL) clouds over the eastern North Atlantic |
title_full |
Environmental effects on aerosol–cloud interaction in non-precipitating marine boundary layer (MBL) clouds over the eastern North Atlantic |
title_fullStr |
Environmental effects on aerosol–cloud interaction in non-precipitating marine boundary layer (MBL) clouds over the eastern North Atlantic |
title_full_unstemmed |
Environmental effects on aerosol–cloud interaction in non-precipitating marine boundary layer (MBL) clouds over the eastern North Atlantic |
title_sort |
environmental effects on aerosol–cloud interaction in non-precipitating marine boundary layer (mbl) clouds over the eastern north atlantic |
publishDate |
2022 |
url |
https://doi.org/10.5194/acp-22-335-2022 https://acp.copernicus.org/articles/22/335/2022/ |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
eISSN: 1680-7324 |
op_relation |
doi:10.5194/acp-22-335-2022 https://acp.copernicus.org/articles/22/335/2022/ |
op_doi |
https://doi.org/10.5194/acp-22-335-2022 |
container_title |
Atmospheric Chemistry and Physics |
container_volume |
22 |
container_issue |
1 |
container_start_page |
335 |
op_container_end_page |
354 |
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1766131314974523392 |