Observation of polar stratospheric clouds over McMurdo (77.85°S, 166.67°E) (2006-2010)

Polar stratospheric clouds (PSCs) have been observed in the Antarctic winter from 2006 to 2010 at the Antarctic base of McMurdo Station using a newly developed Rayleigh lidar. Total backscatter ratio and volume depolarization at 532 nm have been measured from 9 km up to 30 km with an average of 90 m...

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Published in:Journal of Geophysical Research: Atmospheres
Main Author: Di Donfrancesco, G.
Format: Article in Journal/Newspaper
Language:English
Published: 2014
Subjects:
Online Access:https://hdl.handle.net/20.500.12079/2821
https://doi.org/10.1002/2013JD019892
http://www.scopus.com/inward/record.url?eid=2-s2.0-84901707487&partnerID=40&md5=03c923989518c4b320785111348c38bb
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spelling ftenea:oai:iris.enea.it:20.500.12079/2821 2024-04-21T07:48:53+00:00 Observation of polar stratospheric clouds over McMurdo (77.85°S, 166.67°E) (2006-2010) Di Donfrancesco, G. Di Donfrancesco, G. 2014 https://hdl.handle.net/20.500.12079/2821 https://doi.org/10.1002/2013JD019892 http://www.scopus.com/inward/record.url?eid=2-s2.0-84901707487&partnerID=40&md5=03c923989518c4b320785111348c38bb en eng volume:119 issue:9 numberofpages:5528 - 5541 journal:JOURNAL OF GEOPHYSICAL RESEARCH. ATMOSPHERES http://hdl.handle.net/20.500.12079/2821 doi:10.1002/2013JD019892 info:eu-repo/semantics/altIdentifier/scopus/Scopus ID: 2-s2.0-84901707487 http://www.scopus.com/inward/record.url?eid=2-s2.0-84901707487&partnerID=40&md5=03c923989518c4b320785111348c38bb polar stratospheric cloud antarctica tratosphere lidar info:eu-repo/semantics/article 2014 ftenea https://doi.org/20.500.12079/282110.1002/2013JD019892 2024-03-27T15:05:15Z Polar stratospheric clouds (PSCs) have been observed in the Antarctic winter from 2006 to 2010 at the Antarctic base of McMurdo Station using a newly developed Rayleigh lidar. Total backscatter ratio and volume depolarization at 532 nm have been measured from 9 km up to 30 km with an average of 90 measurements per winter season. The data set was analyzed in order to evaluate the occurrence of PSCs based on their altitude, seasonal variability, geometrical thickness, and cloud typology derived from observed optical parameters. We have adopted the latest version of the scheme used to classify PSCs detected by the CALIPSO satellite-based lidar in order to facilitate comparison of ground-based and satellite-borne lidars. This allowed us to approximately identify how processes acting at different spatial scales might affect the formation of different PSC particles. The McMurdo lidar observations are dominated by PSC layers during the Antarctic winter. A clear difference between the different type of PSCs classified according to the observed optical parameters and their geometrical thickness was observed. Ice and supercooled ternary solution PSCs are observed predominantly as thin layers, while thicker layers are associated with nitric acid trihydrate particles. The same classification scheme has been adopted to reanalyze the 1995-2001 McMurdo lidar data in order to compare both data sets (1995-2001 versus 2006-2010). ©2014. American Geophysical Union. All Rights Reserved. Article in Journal/Newspaper Antarc* Antarctic Antarctica ENEA-IRIS Open Archive (Agenzia nazionale per le nuove tecnologie, l'energia e lo sviluppo economico sostenibile) Journal of Geophysical Research: Atmospheres 119 9 5528 5541
institution Open Polar
collection ENEA-IRIS Open Archive (Agenzia nazionale per le nuove tecnologie, l'energia e lo sviluppo economico sostenibile)
op_collection_id ftenea
language English
topic polar stratospheric cloud
antarctica
tratosphere
lidar
spellingShingle polar stratospheric cloud
antarctica
tratosphere
lidar
Di Donfrancesco, G.
Observation of polar stratospheric clouds over McMurdo (77.85°S, 166.67°E) (2006-2010)
topic_facet polar stratospheric cloud
antarctica
tratosphere
lidar
description Polar stratospheric clouds (PSCs) have been observed in the Antarctic winter from 2006 to 2010 at the Antarctic base of McMurdo Station using a newly developed Rayleigh lidar. Total backscatter ratio and volume depolarization at 532 nm have been measured from 9 km up to 30 km with an average of 90 measurements per winter season. The data set was analyzed in order to evaluate the occurrence of PSCs based on their altitude, seasonal variability, geometrical thickness, and cloud typology derived from observed optical parameters. We have adopted the latest version of the scheme used to classify PSCs detected by the CALIPSO satellite-based lidar in order to facilitate comparison of ground-based and satellite-borne lidars. This allowed us to approximately identify how processes acting at different spatial scales might affect the formation of different PSC particles. The McMurdo lidar observations are dominated by PSC layers during the Antarctic winter. A clear difference between the different type of PSCs classified according to the observed optical parameters and their geometrical thickness was observed. Ice and supercooled ternary solution PSCs are observed predominantly as thin layers, while thicker layers are associated with nitric acid trihydrate particles. The same classification scheme has been adopted to reanalyze the 1995-2001 McMurdo lidar data in order to compare both data sets (1995-2001 versus 2006-2010). ©2014. American Geophysical Union. All Rights Reserved.
author2 Di Donfrancesco, G.
format Article in Journal/Newspaper
author Di Donfrancesco, G.
author_facet Di Donfrancesco, G.
author_sort Di Donfrancesco, G.
title Observation of polar stratospheric clouds over McMurdo (77.85°S, 166.67°E) (2006-2010)
title_short Observation of polar stratospheric clouds over McMurdo (77.85°S, 166.67°E) (2006-2010)
title_full Observation of polar stratospheric clouds over McMurdo (77.85°S, 166.67°E) (2006-2010)
title_fullStr Observation of polar stratospheric clouds over McMurdo (77.85°S, 166.67°E) (2006-2010)
title_full_unstemmed Observation of polar stratospheric clouds over McMurdo (77.85°S, 166.67°E) (2006-2010)
title_sort observation of polar stratospheric clouds over mcmurdo (77.85°s, 166.67°e) (2006-2010)
publishDate 2014
url https://hdl.handle.net/20.500.12079/2821
https://doi.org/10.1002/2013JD019892
http://www.scopus.com/inward/record.url?eid=2-s2.0-84901707487&partnerID=40&md5=03c923989518c4b320785111348c38bb
genre Antarc*
Antarctic
Antarctica
genre_facet Antarc*
Antarctic
Antarctica
op_relation volume:119
issue:9
numberofpages:5528 - 5541
journal:JOURNAL OF GEOPHYSICAL RESEARCH. ATMOSPHERES
http://hdl.handle.net/20.500.12079/2821
doi:10.1002/2013JD019892
info:eu-repo/semantics/altIdentifier/scopus/Scopus ID: 2-s2.0-84901707487
http://www.scopus.com/inward/record.url?eid=2-s2.0-84901707487&partnerID=40&md5=03c923989518c4b320785111348c38bb
op_doi https://doi.org/20.500.12079/282110.1002/2013JD019892
container_title Journal of Geophysical Research: Atmospheres
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