Large-eddy simulation of a two-layer boundary-layer cloud system from the Arctic Ocean 2018 expedition
Climate change is particularly noticeable in the Arctic. The most common type of cloud at these latitudes is mixed-phase stratocumulus. These clouds occur frequently and persistently during all seasons and play a critical role in the Arctic energy budget. Previous observations in the central (north...
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ftcopernicus:oai:publications.copernicus.org:acpd108095 2023-05-15T14:48:41+02:00 Large-eddy simulation of a two-layer boundary-layer cloud system from the Arctic Ocean 2018 expedition Bulatovic, Ines Savre, Julien Tjernström, Michael Leck, Caroline Ekman, Annica M. L. 2022-12-20 application/pdf https://doi.org/10.5194/acp-2022-809 https://acp.copernicus.org/preprints/acp-2022-809/ eng eng doi:10.5194/acp-2022-809 https://acp.copernicus.org/preprints/acp-2022-809/ eISSN: 1680-7324 Text 2022 ftcopernicus https://doi.org/10.5194/acp-2022-809 2022-12-26T17:22:42Z Climate change is particularly noticeable in the Arctic. The most common type of cloud at these latitudes is mixed-phase stratocumulus. These clouds occur frequently and persistently during all seasons and play a critical role in the Arctic energy budget. Previous observations in the central (north of 80° N) Arctic have shown a high occurrence of prolonged periods of a shallow, single-layer mixed-phase stratocumulus at the top of the boundary layer (BL; altitudes ~300 to 400 m). However, recent observations from the summer of 2018 instead showed a prevalence of a two-layer boundary-layer cloud system. Here we use large-eddy simulation to examine the maintenance of one of the cloud systems observed in the summer of 2018 as well as the sensitivity of the cloud layers to different micro- and macro-scale parameters. We find that the model generally reproduces the observed thermodynamic structure well, with two near-neutrally stratified layers in the BL caused by a low cloud (located within the first few hundred meters) capped by a lower temperature inversion, and an upper cloud layer (based around one km or slightly higher) capped by the main temperature inversion of the BL. The investigated cloud structure is persistent unless there are low aerosol number concentrations (≤ 5 cm -3 ), which cause the upper cloud layer to dissipate, or high large-scale wind speeds (greater than or equal 8.5 m s -1 ), which erode the lower inversion and the related cloud layer. These types of changes in cloud structure lead to a substantial reduction of the net longwave radiation at the surface due to a lower emissivity or higher altitude of the remaining cloud layer. The findings highlight the importance of better understanding and representing aerosol sources and sinks over the central Arctic Ocean. Furthermore, they underline the significance of meteorological parameters, such as the large-scale wind speed, for maintaining the two-layer boundary-layer cloud structure encountered in the lower atmosphere of the central Arctic. Text Arctic Arctic Ocean Climate change Copernicus Publications: E-Journals Arctic Arctic Ocean |
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Open Polar |
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Copernicus Publications: E-Journals |
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ftcopernicus |
language |
English |
description |
Climate change is particularly noticeable in the Arctic. The most common type of cloud at these latitudes is mixed-phase stratocumulus. These clouds occur frequently and persistently during all seasons and play a critical role in the Arctic energy budget. Previous observations in the central (north of 80° N) Arctic have shown a high occurrence of prolonged periods of a shallow, single-layer mixed-phase stratocumulus at the top of the boundary layer (BL; altitudes ~300 to 400 m). However, recent observations from the summer of 2018 instead showed a prevalence of a two-layer boundary-layer cloud system. Here we use large-eddy simulation to examine the maintenance of one of the cloud systems observed in the summer of 2018 as well as the sensitivity of the cloud layers to different micro- and macro-scale parameters. We find that the model generally reproduces the observed thermodynamic structure well, with two near-neutrally stratified layers in the BL caused by a low cloud (located within the first few hundred meters) capped by a lower temperature inversion, and an upper cloud layer (based around one km or slightly higher) capped by the main temperature inversion of the BL. The investigated cloud structure is persistent unless there are low aerosol number concentrations (≤ 5 cm -3 ), which cause the upper cloud layer to dissipate, or high large-scale wind speeds (greater than or equal 8.5 m s -1 ), which erode the lower inversion and the related cloud layer. These types of changes in cloud structure lead to a substantial reduction of the net longwave radiation at the surface due to a lower emissivity or higher altitude of the remaining cloud layer. The findings highlight the importance of better understanding and representing aerosol sources and sinks over the central Arctic Ocean. Furthermore, they underline the significance of meteorological parameters, such as the large-scale wind speed, for maintaining the two-layer boundary-layer cloud structure encountered in the lower atmosphere of the central Arctic. |
format |
Text |
author |
Bulatovic, Ines Savre, Julien Tjernström, Michael Leck, Caroline Ekman, Annica M. L. |
spellingShingle |
Bulatovic, Ines Savre, Julien Tjernström, Michael Leck, Caroline Ekman, Annica M. L. Large-eddy simulation of a two-layer boundary-layer cloud system from the Arctic Ocean 2018 expedition |
author_facet |
Bulatovic, Ines Savre, Julien Tjernström, Michael Leck, Caroline Ekman, Annica M. L. |
author_sort |
Bulatovic, Ines |
title |
Large-eddy simulation of a two-layer boundary-layer cloud system from the Arctic Ocean 2018 expedition |
title_short |
Large-eddy simulation of a two-layer boundary-layer cloud system from the Arctic Ocean 2018 expedition |
title_full |
Large-eddy simulation of a two-layer boundary-layer cloud system from the Arctic Ocean 2018 expedition |
title_fullStr |
Large-eddy simulation of a two-layer boundary-layer cloud system from the Arctic Ocean 2018 expedition |
title_full_unstemmed |
Large-eddy simulation of a two-layer boundary-layer cloud system from the Arctic Ocean 2018 expedition |
title_sort |
large-eddy simulation of a two-layer boundary-layer cloud system from the arctic ocean 2018 expedition |
publishDate |
2022 |
url |
https://doi.org/10.5194/acp-2022-809 https://acp.copernicus.org/preprints/acp-2022-809/ |
geographic |
Arctic Arctic Ocean |
geographic_facet |
Arctic Arctic Ocean |
genre |
Arctic Arctic Ocean Climate change |
genre_facet |
Arctic Arctic Ocean Climate change |
op_source |
eISSN: 1680-7324 |
op_relation |
doi:10.5194/acp-2022-809 https://acp.copernicus.org/preprints/acp-2022-809/ |
op_doi |
https://doi.org/10.5194/acp-2022-809 |
_version_ |
1766319769272713216 |