Detection of particles layers in backscatter profiles: application to Antarctic lidar measurements

A detection method is proposed and studied to infer the presence of hidden signals in a statistical way. It is applied here to the detection of Polar Stratospheric Clouds (PSC) layers in lidar backscatter profiles measured over the Dumont D'Urville station (Antarctica). PSCs appear as layers wi...

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Published in:Atmospheric Chemistry and Physics
Main Authors: Gazeaux, Julien, Bekki, Slimane, Naveau, Philippe, Keckhut, Philippe, Jumelet, Julien, Paredes, José, David, Christine
Other Authors: STRATO - LATMOS, Laboratoire Atmosphères, Milieux, Observations Spatiales (LATMOS), Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ), Extrèmes : Statistiques, Impacts et Régionalisation (ESTIMR), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2012
Subjects:
Online Access:https://hal.archives-ouvertes.fr/hal-00613735
https://hal.archives-ouvertes.fr/hal-00613735/document
https://hal.archives-ouvertes.fr/hal-00613735/file/acp-12-3205-2012.pdf
https://doi.org/10.5194/acp-12-3205-2012
id ftccsdartic:oai:HAL:hal-00613735v1
record_format openpolar
institution Open Polar
collection Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe)
op_collection_id ftccsdartic
language English
topic [PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph]
spellingShingle [PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph]
Gazeaux, Julien
Bekki, Slimane
Naveau, Philippe
Keckhut, Philippe
Jumelet, Julien
Paredes, José
David, Christine
Detection of particles layers in backscatter profiles: application to Antarctic lidar measurements
topic_facet [PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph]
description A detection method is proposed and studied to infer the presence of hidden signals in a statistical way. It is applied here to the detection of Polar Stratospheric Clouds (PSC) layers in lidar backscatter profiles measured over the Dumont D'Urville station (Antarctica). PSCs appear as layers with enhanced variance in non stationary, heteroscedastic signal profiles, between two unknown altitudes to be estimated. The method is based on a three step algorithm. The first step is the stationarization of the signal, the second performs the maximum likelihoods estimation of the signal (PSC altitude range and variance inside and outside the PSC layer). The last step uses a Fisher-Snédécor test to decide whether the detection of PSC layer is statistically significant. Performances and robustness of the method are tested on simulated data with given statistical properties. Bias and detection limit are estimated. The method is then applied to lidar backscatter profiles measured in 2008. No PSC are detected during seasons when PSCs are not expected to form. As expected, PSC layers are detected during the austral winter and early spring. The effect of time averaging of the profiles is investigated. The best compromise for detection of PSC layers in lidar backscatter profiles acquired at Dumont D'Urville is a time averaging window of 1 hour typically.
author2 STRATO - LATMOS
Laboratoire Atmosphères, Milieux, Observations Spatiales (LATMOS)
Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)
Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE)
Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)
Extrèmes : Statistiques, Impacts et Régionalisation (ESTIMR)
Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)
format Article in Journal/Newspaper
author Gazeaux, Julien
Bekki, Slimane
Naveau, Philippe
Keckhut, Philippe
Jumelet, Julien
Paredes, José
David, Christine
author_facet Gazeaux, Julien
Bekki, Slimane
Naveau, Philippe
Keckhut, Philippe
Jumelet, Julien
Paredes, José
David, Christine
author_sort Gazeaux, Julien
title Detection of particles layers in backscatter profiles: application to Antarctic lidar measurements
title_short Detection of particles layers in backscatter profiles: application to Antarctic lidar measurements
title_full Detection of particles layers in backscatter profiles: application to Antarctic lidar measurements
title_fullStr Detection of particles layers in backscatter profiles: application to Antarctic lidar measurements
title_full_unstemmed Detection of particles layers in backscatter profiles: application to Antarctic lidar measurements
title_sort detection of particles layers in backscatter profiles: application to antarctic lidar measurements
publisher HAL CCSD
publishDate 2012
url https://hal.archives-ouvertes.fr/hal-00613735
https://hal.archives-ouvertes.fr/hal-00613735/document
https://hal.archives-ouvertes.fr/hal-00613735/file/acp-12-3205-2012.pdf
https://doi.org/10.5194/acp-12-3205-2012
long_lat ENVELOPE(140.017,140.017,-66.667,-66.667)
ENVELOPE(140.013,140.013,-66.667,-66.667)
ENVELOPE(140.000,140.000,-66.667,-66.667)
geographic Antarctic
Austral
Dumont d'Urville
Dumont-d'Urville
Dumont d'Urville Station
geographic_facet Antarctic
Austral
Dumont d'Urville
Dumont-d'Urville
Dumont d'Urville Station
genre Antarc*
Antarctic
Antarctica
genre_facet Antarc*
Antarctic
Antarctica
op_source ISSN: 1680-7316
EISSN: 1680-7324
Atmospheric Chemistry and Physics
https://hal.archives-ouvertes.fr/hal-00613735
Atmospheric Chemistry and Physics, European Geosciences Union, 2012, 12 (7), pp.3205-3217. ⟨10.5194/acp-12-3205-2012⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.5194/acp-12-3205-2012
hal-00613735
https://hal.archives-ouvertes.fr/hal-00613735
https://hal.archives-ouvertes.fr/hal-00613735/document
https://hal.archives-ouvertes.fr/hal-00613735/file/acp-12-3205-2012.pdf
doi:10.5194/acp-12-3205-2012
op_rights info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.5194/acp-12-3205-2012
container_title Atmospheric Chemistry and Physics
container_volume 12
container_issue 7
container_start_page 3205
op_container_end_page 3217
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spelling ftccsdartic:oai:HAL:hal-00613735v1 2023-05-15T13:33:47+02:00 Detection of particles layers in backscatter profiles: application to Antarctic lidar measurements Gazeaux, Julien Bekki, Slimane Naveau, Philippe Keckhut, Philippe Jumelet, Julien Paredes, José David, Christine STRATO - LATMOS Laboratoire Atmosphères, Milieux, Observations Spatiales (LATMOS) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS) Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE) Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ) Extrèmes : Statistiques, Impacts et Régionalisation (ESTIMR) Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ) 2012 https://hal.archives-ouvertes.fr/hal-00613735 https://hal.archives-ouvertes.fr/hal-00613735/document https://hal.archives-ouvertes.fr/hal-00613735/file/acp-12-3205-2012.pdf https://doi.org/10.5194/acp-12-3205-2012 en eng HAL CCSD European Geosciences Union info:eu-repo/semantics/altIdentifier/doi/10.5194/acp-12-3205-2012 hal-00613735 https://hal.archives-ouvertes.fr/hal-00613735 https://hal.archives-ouvertes.fr/hal-00613735/document https://hal.archives-ouvertes.fr/hal-00613735/file/acp-12-3205-2012.pdf doi:10.5194/acp-12-3205-2012 info:eu-repo/semantics/OpenAccess ISSN: 1680-7316 EISSN: 1680-7324 Atmospheric Chemistry and Physics https://hal.archives-ouvertes.fr/hal-00613735 Atmospheric Chemistry and Physics, European Geosciences Union, 2012, 12 (7), pp.3205-3217. ⟨10.5194/acp-12-3205-2012⟩ [PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph] info:eu-repo/semantics/article Journal articles 2012 ftccsdartic https://doi.org/10.5194/acp-12-3205-2012 2021-12-19T02:52:45Z A detection method is proposed and studied to infer the presence of hidden signals in a statistical way. It is applied here to the detection of Polar Stratospheric Clouds (PSC) layers in lidar backscatter profiles measured over the Dumont D'Urville station (Antarctica). PSCs appear as layers with enhanced variance in non stationary, heteroscedastic signal profiles, between two unknown altitudes to be estimated. The method is based on a three step algorithm. The first step is the stationarization of the signal, the second performs the maximum likelihoods estimation of the signal (PSC altitude range and variance inside and outside the PSC layer). The last step uses a Fisher-Snédécor test to decide whether the detection of PSC layer is statistically significant. Performances and robustness of the method are tested on simulated data with given statistical properties. Bias and detection limit are estimated. The method is then applied to lidar backscatter profiles measured in 2008. No PSC are detected during seasons when PSCs are not expected to form. As expected, PSC layers are detected during the austral winter and early spring. The effect of time averaging of the profiles is investigated. The best compromise for detection of PSC layers in lidar backscatter profiles acquired at Dumont D'Urville is a time averaging window of 1 hour typically. Article in Journal/Newspaper Antarc* Antarctic Antarctica Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) Antarctic Austral Dumont d'Urville ENVELOPE(140.017,140.017,-66.667,-66.667) Dumont-d'Urville ENVELOPE(140.013,140.013,-66.667,-66.667) Dumont d'Urville Station ENVELOPE(140.000,140.000,-66.667,-66.667) Atmospheric Chemistry and Physics 12 7 3205 3217