On the relationship between mesoscale cellular convection and meteorological forcing: Comparing the Southern Ocean against the North Pacific

Marine atmospheric boundary layer (MABL) clouds cover vast areas over the ocean and have important radiative effects on the Earth’s climate system. These radiative effects are known to be sensitive to the local organization, or structure, of the mesoscale cellular convection (MCC). A convolution neu...

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Main Authors: Lang, Francisco, Siems, Steven T., Huang, Yi, Ackermann, Luis
Format: Text
Language:English
Published: 2023
Subjects:
Online Access:https://doi.org/10.5194/egusphere-2023-518
https://egusphere.copernicus.org/preprints/2023/egusphere-2023-518/
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spelling ftcopernicus:oai:publications.copernicus.org:egusphere110275 2023-06-06T11:59:32+02:00 On the relationship between mesoscale cellular convection and meteorological forcing: Comparing the Southern Ocean against the North Pacific Lang, Francisco Siems, Steven T. Huang, Yi Ackermann, Luis 2023-04-11 application/pdf https://doi.org/10.5194/egusphere-2023-518 https://egusphere.copernicus.org/preprints/2023/egusphere-2023-518/ eng eng doi:10.5194/egusphere-2023-518 https://egusphere.copernicus.org/preprints/2023/egusphere-2023-518/ eISSN: Text 2023 ftcopernicus https://doi.org/10.5194/egusphere-2023-518 2023-04-17T16:23:12Z Marine atmospheric boundary layer (MABL) clouds cover vast areas over the ocean and have important radiative effects on the Earth’s climate system. These radiative effects are known to be sensitive to the local organization, or structure, of the mesoscale cellular convection (MCC). A convolution neural network model is used to identify the two ideal classes of MCC clouds, namely open and closed, over the Southern Ocean (SO) and Northwest Pacific (NP) from high-frequency geostationary Himawari-8 satellite observations. The results of the climatology show that MCC clouds are roughly distributed over the midlatitude storm tracks for both hemispheres, with peaks poleward of the 40° latitude. Open MCC clouds are more prevalent than closed MCC in both regions. An examination of meteorological forcing associated with open and closed MCC clouds is conducted to illustrate the influence of large-scale meteorological conditions. We establish the importance of the Kuroshio western boundary current in the spatial coverage of open and closed MCC across the NP, presumably through the supply of strong heat and moisture fluxes during marine cold air outbreaks events. For both regions, closed MCC cloud are more frequent at higher static stability than on air-sea temperature difference, opposite to the open MCC cloud behavior. The diurnal cycle reveals a pronounced daily cycle in the frequency of occurrence of closed MCC over the SO, while the NP closed MCC daily cycle is less noticeable. Text Southern Ocean Copernicus Publications: E-Journals Pacific Southern Ocean
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description Marine atmospheric boundary layer (MABL) clouds cover vast areas over the ocean and have important radiative effects on the Earth’s climate system. These radiative effects are known to be sensitive to the local organization, or structure, of the mesoscale cellular convection (MCC). A convolution neural network model is used to identify the two ideal classes of MCC clouds, namely open and closed, over the Southern Ocean (SO) and Northwest Pacific (NP) from high-frequency geostationary Himawari-8 satellite observations. The results of the climatology show that MCC clouds are roughly distributed over the midlatitude storm tracks for both hemispheres, with peaks poleward of the 40° latitude. Open MCC clouds are more prevalent than closed MCC in both regions. An examination of meteorological forcing associated with open and closed MCC clouds is conducted to illustrate the influence of large-scale meteorological conditions. We establish the importance of the Kuroshio western boundary current in the spatial coverage of open and closed MCC across the NP, presumably through the supply of strong heat and moisture fluxes during marine cold air outbreaks events. For both regions, closed MCC cloud are more frequent at higher static stability than on air-sea temperature difference, opposite to the open MCC cloud behavior. The diurnal cycle reveals a pronounced daily cycle in the frequency of occurrence of closed MCC over the SO, while the NP closed MCC daily cycle is less noticeable.
format Text
author Lang, Francisco
Siems, Steven T.
Huang, Yi
Ackermann, Luis
spellingShingle Lang, Francisco
Siems, Steven T.
Huang, Yi
Ackermann, Luis
On the relationship between mesoscale cellular convection and meteorological forcing: Comparing the Southern Ocean against the North Pacific
author_facet Lang, Francisco
Siems, Steven T.
Huang, Yi
Ackermann, Luis
author_sort Lang, Francisco
title On the relationship between mesoscale cellular convection and meteorological forcing: Comparing the Southern Ocean against the North Pacific
title_short On the relationship between mesoscale cellular convection and meteorological forcing: Comparing the Southern Ocean against the North Pacific
title_full On the relationship between mesoscale cellular convection and meteorological forcing: Comparing the Southern Ocean against the North Pacific
title_fullStr On the relationship between mesoscale cellular convection and meteorological forcing: Comparing the Southern Ocean against the North Pacific
title_full_unstemmed On the relationship between mesoscale cellular convection and meteorological forcing: Comparing the Southern Ocean against the North Pacific
title_sort on the relationship between mesoscale cellular convection and meteorological forcing: comparing the southern ocean against the north pacific
publishDate 2023
url https://doi.org/10.5194/egusphere-2023-518
https://egusphere.copernicus.org/preprints/2023/egusphere-2023-518/
geographic Pacific
Southern Ocean
geographic_facet Pacific
Southern Ocean
genre Southern Ocean
genre_facet Southern Ocean
op_source eISSN:
op_relation doi:10.5194/egusphere-2023-518
https://egusphere.copernicus.org/preprints/2023/egusphere-2023-518/
op_doi https://doi.org/10.5194/egusphere-2023-518
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