Antarctic cloud macrophysical, thermodynamic phase, and atmospheric inversion coupling properties at McMurdo Station. Part II: Radiative impact during different synoptic regimes
Different cloud types are generated over Antarctica as a result of various synoptic conditions. The cloud characteristics affect their impact on the surface energy budget. In this study, the dominating synoptic regimes over Antarctica (centered on the Ross Ice Shelf) are classified using self-organi...
Published in: | Journal of Geophysical Research: Atmospheres |
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Online Access: | http://www.osti.gov/servlets/purl/1491701 https://www.osti.gov/biblio/1491701 https://doi.org/10.1029/2018JD029471 |
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ftosti:oai:osti.gov:1491701 2023-07-30T03:58:33+02:00 Antarctic cloud macrophysical, thermodynamic phase, and atmospheric inversion coupling properties at McMurdo Station. Part II: Radiative impact during different synoptic regimes Silber, Israel Vogelmann, Andrew M. Verlinde, Johannes Cadeddu, Maria Flynn, Connor J. Eloranta, Edwin W. 2021-08-30 application/pdf http://www.osti.gov/servlets/purl/1491701 https://www.osti.gov/biblio/1491701 https://doi.org/10.1029/2018JD029471 unknown http://www.osti.gov/servlets/purl/1491701 https://www.osti.gov/biblio/1491701 https://doi.org/10.1029/2018JD029471 doi:10.1029/2018JD029471 54 ENVIRONMENTAL SCIENCES 2021 ftosti https://doi.org/10.1029/2018JD029471 2023-07-11T09:31:02Z Different cloud types are generated over Antarctica as a result of various synoptic conditions. The cloud characteristics affect their impact on the surface energy budget. In this study, the dominating synoptic regimes over Antarctica (centered on the Ross Ice Shelf) are classified using self-organizing map (SOM) analysis, applied over long-term ERA-Interim 700 hPa geopotential height data. The corresponding cloud properties over McMurdo Station (measured as part of the AWARE campaign) are described and discussed with respect to the synoptic settings and sea-ice extent conditions. Cloud radiative forcing calculations are performed as well, and a particular focus is given to the net longwave “radiatively cloudy/opaque” (RO) regime. These results are compared with measurements performed at the West Antarctic Ice Sheet (WAIS) Divide to examine their variability and applicability to other Antarctic locations. It is found that the McMurdo cloud properties are strongly affected by the regional flow patterns and mesoscale cyclonic activity, which often moderates the larger-scale synoptic regime influence. In contrast, the WAIS clouds are more susceptible to the varying synoptic settings. Furthermore, it is suggested that the positive trend in the (frequent) cyclonic activity near the Antarctic coastal regions makes ice-clouds an increasingly prominent contributor for the RO cases, especially during freeze-up and maximum sea-ice conditions. Other/Unknown Material Antarc* Antarctic Antarctica Ice Sheet Ice Shelf Ross Ice Shelf Sea ice SciTec Connect (Office of Scientific and Technical Information - OSTI, U.S. Department of Energy) Antarctic The Antarctic West Antarctic Ice Sheet Ross Ice Shelf McMurdo Station ENVELOPE(166.667,166.667,-77.850,-77.850) Journal of Geophysical Research: Atmospheres 124 3 1697 1719 |
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SciTec Connect (Office of Scientific and Technical Information - OSTI, U.S. Department of Energy) |
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ftosti |
language |
unknown |
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54 ENVIRONMENTAL SCIENCES |
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54 ENVIRONMENTAL SCIENCES Silber, Israel Vogelmann, Andrew M. Verlinde, Johannes Cadeddu, Maria Flynn, Connor J. Eloranta, Edwin W. Antarctic cloud macrophysical, thermodynamic phase, and atmospheric inversion coupling properties at McMurdo Station. Part II: Radiative impact during different synoptic regimes |
topic_facet |
54 ENVIRONMENTAL SCIENCES |
description |
Different cloud types are generated over Antarctica as a result of various synoptic conditions. The cloud characteristics affect their impact on the surface energy budget. In this study, the dominating synoptic regimes over Antarctica (centered on the Ross Ice Shelf) are classified using self-organizing map (SOM) analysis, applied over long-term ERA-Interim 700 hPa geopotential height data. The corresponding cloud properties over McMurdo Station (measured as part of the AWARE campaign) are described and discussed with respect to the synoptic settings and sea-ice extent conditions. Cloud radiative forcing calculations are performed as well, and a particular focus is given to the net longwave “radiatively cloudy/opaque” (RO) regime. These results are compared with measurements performed at the West Antarctic Ice Sheet (WAIS) Divide to examine their variability and applicability to other Antarctic locations. It is found that the McMurdo cloud properties are strongly affected by the regional flow patterns and mesoscale cyclonic activity, which often moderates the larger-scale synoptic regime influence. In contrast, the WAIS clouds are more susceptible to the varying synoptic settings. Furthermore, it is suggested that the positive trend in the (frequent) cyclonic activity near the Antarctic coastal regions makes ice-clouds an increasingly prominent contributor for the RO cases, especially during freeze-up and maximum sea-ice conditions. |
author |
Silber, Israel Vogelmann, Andrew M. Verlinde, Johannes Cadeddu, Maria Flynn, Connor J. Eloranta, Edwin W. |
author_facet |
Silber, Israel Vogelmann, Andrew M. Verlinde, Johannes Cadeddu, Maria Flynn, Connor J. Eloranta, Edwin W. |
author_sort |
Silber, Israel |
title |
Antarctic cloud macrophysical, thermodynamic phase, and atmospheric inversion coupling properties at McMurdo Station. Part II: Radiative impact during different synoptic regimes |
title_short |
Antarctic cloud macrophysical, thermodynamic phase, and atmospheric inversion coupling properties at McMurdo Station. Part II: Radiative impact during different synoptic regimes |
title_full |
Antarctic cloud macrophysical, thermodynamic phase, and atmospheric inversion coupling properties at McMurdo Station. Part II: Radiative impact during different synoptic regimes |
title_fullStr |
Antarctic cloud macrophysical, thermodynamic phase, and atmospheric inversion coupling properties at McMurdo Station. Part II: Radiative impact during different synoptic regimes |
title_full_unstemmed |
Antarctic cloud macrophysical, thermodynamic phase, and atmospheric inversion coupling properties at McMurdo Station. Part II: Radiative impact during different synoptic regimes |
title_sort |
antarctic cloud macrophysical, thermodynamic phase, and atmospheric inversion coupling properties at mcmurdo station. part ii: radiative impact during different synoptic regimes |
publishDate |
2021 |
url |
http://www.osti.gov/servlets/purl/1491701 https://www.osti.gov/biblio/1491701 https://doi.org/10.1029/2018JD029471 |
long_lat |
ENVELOPE(166.667,166.667,-77.850,-77.850) |
geographic |
Antarctic The Antarctic West Antarctic Ice Sheet Ross Ice Shelf McMurdo Station |
geographic_facet |
Antarctic The Antarctic West Antarctic Ice Sheet Ross Ice Shelf McMurdo Station |
genre |
Antarc* Antarctic Antarctica Ice Sheet Ice Shelf Ross Ice Shelf Sea ice |
genre_facet |
Antarc* Antarctic Antarctica Ice Sheet Ice Shelf Ross Ice Shelf Sea ice |
op_relation |
http://www.osti.gov/servlets/purl/1491701 https://www.osti.gov/biblio/1491701 https://doi.org/10.1029/2018JD029471 doi:10.1029/2018JD029471 |
op_doi |
https://doi.org/10.1029/2018JD029471 |
container_title |
Journal of Geophysical Research: Atmospheres |
container_volume |
124 |
container_issue |
3 |
container_start_page |
1697 |
op_container_end_page |
1719 |
_version_ |
1772821326320369664 |