Inâ€cloud variability of LIDAR depolarization of polar and midlatitude cirrus
LIDAR depolarization is commonly used for discriminating liquid and ice particles. Since depolarization depends in a complicated manner on particle shape and size, inâ€cloud variability of depolarization has been used as an indicator of the microphysical homogeneity of cirrus. The comparison between...
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2003
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Online Access: | https://www.openaccessrepository.it/record/189352 https://doi.org/10.1029/2003gl017163 |
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ftopenaccessrep:oai:zenodo.org:189352 2024-05-12T07:53:35+00:00 Inâ€cloud variability of LIDAR depolarization of polar and midlatitude cirrus Del Guasta, Massimo Vallar, Edgar 2003-06-12 https://www.openaccessrepository.it/record/189352 https://doi.org/10.1029/2003gl017163 eng eng url:https://www.openaccessrepository.it/communities/itmirror https://www.openaccessrepository.it/record/189352 doi:10.1029/2003gl017163 info:eu-repo/semantics/openAccess General Earth and Planetary Sciences Geophysics info:eu-repo/semantics/article publication-article 2003 ftopenaccessrep https://doi.org/10.1029/2003gl017163 2024-04-17T15:08:34Z LIDAR depolarization is commonly used for discriminating liquid and ice particles. Since depolarization depends in a complicated manner on particle shape and size, inâ€cloud variability of depolarization has been used as an indicator of the microphysical homogeneity of cirrus. The comparison between midlatitude (Florence, Italy, 43. 60°N) and polar (Dumont d'Urville, Antarctica, 66. 68°S) cirrus showed a lower mean depolarization and a higher inâ€cloud uniformity of cloud depolarization for polar clouds in the (−80, −50°C) temperature range. A wider inâ€cloud variability of depolarization was observed in polar clouds at higher temperatures (−50, −30°C), reflecting the presence of supercooled liquid layers. The large inâ€cloud variability of depolarization in Florence cirrus could be explained with a microphysics that is dynamically and chemically perturbed as compared with the polar site. Aged jet contrails are, in fact, present in many Florence cirrus records. Article in Journal/Newspaper Antarc* Antarctica Istituto Nazionale di Fisica Nucleare (INFN): Open Access Repository Dumont d'Urville ENVELOPE(140.017,140.017,-66.667,-66.667) Dumont-d'Urville ENVELOPE(140.013,140.013,-66.667,-66.667) Geophysical Research Letters 30 11 |
institution |
Open Polar |
collection |
Istituto Nazionale di Fisica Nucleare (INFN): Open Access Repository |
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ftopenaccessrep |
language |
English |
topic |
General Earth and Planetary Sciences Geophysics |
spellingShingle |
General Earth and Planetary Sciences Geophysics Del Guasta, Massimo Vallar, Edgar Inâ€cloud variability of LIDAR depolarization of polar and midlatitude cirrus |
topic_facet |
General Earth and Planetary Sciences Geophysics |
description |
LIDAR depolarization is commonly used for discriminating liquid and ice particles. Since depolarization depends in a complicated manner on particle shape and size, inâ€cloud variability of depolarization has been used as an indicator of the microphysical homogeneity of cirrus. The comparison between midlatitude (Florence, Italy, 43. 60°N) and polar (Dumont d'Urville, Antarctica, 66. 68°S) cirrus showed a lower mean depolarization and a higher inâ€cloud uniformity of cloud depolarization for polar clouds in the (−80, −50°C) temperature range. A wider inâ€cloud variability of depolarization was observed in polar clouds at higher temperatures (−50, −30°C), reflecting the presence of supercooled liquid layers. The large inâ€cloud variability of depolarization in Florence cirrus could be explained with a microphysics that is dynamically and chemically perturbed as compared with the polar site. Aged jet contrails are, in fact, present in many Florence cirrus records. |
format |
Article in Journal/Newspaper |
author |
Del Guasta, Massimo Vallar, Edgar |
author_facet |
Del Guasta, Massimo Vallar, Edgar |
author_sort |
Del Guasta, Massimo |
title |
Inâ€cloud variability of LIDAR depolarization of polar and midlatitude cirrus |
title_short |
Inâ€cloud variability of LIDAR depolarization of polar and midlatitude cirrus |
title_full |
Inâ€cloud variability of LIDAR depolarization of polar and midlatitude cirrus |
title_fullStr |
Inâ€cloud variability of LIDAR depolarization of polar and midlatitude cirrus |
title_full_unstemmed |
Inâ€cloud variability of LIDAR depolarization of polar and midlatitude cirrus |
title_sort |
inâ€cloud variability of lidar depolarization of polar and midlatitude cirrus |
publishDate |
2003 |
url |
https://www.openaccessrepository.it/record/189352 https://doi.org/10.1029/2003gl017163 |
long_lat |
ENVELOPE(140.017,140.017,-66.667,-66.667) ENVELOPE(140.013,140.013,-66.667,-66.667) |
geographic |
Dumont d'Urville Dumont-d'Urville |
geographic_facet |
Dumont d'Urville Dumont-d'Urville |
genre |
Antarc* Antarctica |
genre_facet |
Antarc* Antarctica |
op_relation |
url:https://www.openaccessrepository.it/communities/itmirror https://www.openaccessrepository.it/record/189352 doi:10.1029/2003gl017163 |
op_rights |
info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1029/2003gl017163 |
container_title |
Geophysical Research Letters |
container_volume |
30 |
container_issue |
11 |
_version_ |
1798843467634311168 |