Springtime aerosol load as observed from ground-based and airborne lidars over northern Norway

International audience To investigate the origin of springtime aerosols in the Arctic region we performed ground-based and airborne 355nm Raman lidar observations in the north of Norway (Hammerfest). Two lidars were embedded (i) on an ultralight aircraft for vertical (nadir) or horizontal line-of-si...

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Published in:Atmospheric Chemistry and Physics
Main Authors: Chazette, Patrick, Raut, Jean-Christophe, Totems, Julien
Other Authors: 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), Chimie Atmosphérique Expérimentale (CAE), 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), TROPO - LATMOS, Laboratoire Atmosphères, Milieux, Observations Spatiales (LATMOS), Sorbonne Université (SU)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2018
Subjects:
Online Access:https://hal-insu.archives-ouvertes.fr/insu-01808641
https://hal-insu.archives-ouvertes.fr/insu-01808641/document
https://hal-insu.archives-ouvertes.fr/insu-01808641/file/acp-18-13075-2018.pdf
https://doi.org/10.5194/acp-18-13075-2018
id ftccsdartic:oai:HAL:insu-01808641v1
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]
Chazette, Patrick
Raut, Jean-Christophe
Totems, Julien
Springtime aerosol load as observed from ground-based and airborne lidars over northern Norway
topic_facet [PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph]
description International audience To investigate the origin of springtime aerosols in the Arctic region we performed ground-based and airborne 355nm Raman lidar observations in the north of Norway (Hammerfest). Two lidars were embedded (i) on an ultralight aircraft for vertical (nadir) or horizontal line-of-sight measurements and (ii) in an air-conditioned van on the ground for vertical (zenith) measurements. This field experiment was designed as part of the Pollution in the ARCtic System (PARCS) project of the French Arctic Initiative and took place from 13 to 26 May 2016. The consistency among lidar measurements is verified by comparing nadir, horizontal line of sight, and ground-based Raman lidar profiles. Dispersion of the order of 0.01km −1 is obtained among lidar-derived aerosol extinction coefficients at 355nm. The aerosol load measured in the first 3km of the troposphere remains low throughout the campaign, with aerosol optical thickness (AOT) of 0.1 at 355nm ( ∼ 0.05 at 550nm). The main contributors to the evolution of the aerosol load at low altitude prove to be one of the flares of the nearby Melkøya gas processing facility, the oceanic source, and the transport of aerosols from industrial sites in Russia. Moreover, ground-based lidar measurements allowed us to identify three cases of long-range aerosol transport (between 3 and 8km above the mean sea level). Using back trajectories computed with the Lagrangian model FLEXPART-WRF, these aerosol plumes are shown to be the result of the strong forest fires that occurred in the area of Fort McMurray, in Canada. They can at most double the AOT value over the Arctic area, with an anomaly of 0.1 on the AOT at 355nm.
author2 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)
Chimie Atmosphérique Expérimentale (CAE)
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)
TROPO - LATMOS
Laboratoire Atmosphères, Milieux, Observations Spatiales (LATMOS)
Sorbonne Université (SU)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)
format Article in Journal/Newspaper
author Chazette, Patrick
Raut, Jean-Christophe
Totems, Julien
author_facet Chazette, Patrick
Raut, Jean-Christophe
Totems, Julien
author_sort Chazette, Patrick
title Springtime aerosol load as observed from ground-based and airborne lidars over northern Norway
title_short Springtime aerosol load as observed from ground-based and airborne lidars over northern Norway
title_full Springtime aerosol load as observed from ground-based and airborne lidars over northern Norway
title_fullStr Springtime aerosol load as observed from ground-based and airborne lidars over northern Norway
title_full_unstemmed Springtime aerosol load as observed from ground-based and airborne lidars over northern Norway
title_sort springtime aerosol load as observed from ground-based and airborne lidars over northern norway
publisher HAL CCSD
publishDate 2018
url https://hal-insu.archives-ouvertes.fr/insu-01808641
https://hal-insu.archives-ouvertes.fr/insu-01808641/document
https://hal-insu.archives-ouvertes.fr/insu-01808641/file/acp-18-13075-2018.pdf
https://doi.org/10.5194/acp-18-13075-2018
geographic Arctic
Fort McMurray
Canada
Norway
geographic_facet Arctic
Fort McMurray
Canada
Norway
genre Arctic
Fort McMurray
Hammerfest
Northern Norway
genre_facet Arctic
Fort McMurray
Hammerfest
Northern Norway
op_source ISSN: 1680-7316
EISSN: 1680-7324
Atmospheric Chemistry and Physics
https://hal-insu.archives-ouvertes.fr/insu-01808641
Atmospheric Chemistry and Physics, European Geosciences Union, 2018, 18, pp.13075-13095. ⟨10.5194/acp-18-13075-2018⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.5194/acp-18-13075-2018
insu-01808641
https://hal-insu.archives-ouvertes.fr/insu-01808641
https://hal-insu.archives-ouvertes.fr/insu-01808641/document
https://hal-insu.archives-ouvertes.fr/insu-01808641/file/acp-18-13075-2018.pdf
doi:10.5194/acp-18-13075-2018
op_rights info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.5194/acp-18-13075-2018
container_title Atmospheric Chemistry and Physics
container_volume 18
container_issue 17
container_start_page 13075
op_container_end_page 13095
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spelling ftccsdartic:oai:HAL:insu-01808641v1 2023-05-15T14:51:59+02:00 Springtime aerosol load as observed from ground-based and airborne lidars over northern Norway Chazette, Patrick Raut, Jean-Christophe Totems, Julien 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) Chimie Atmosphérique Expérimentale (CAE) 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) TROPO - LATMOS Laboratoire Atmosphères, Milieux, Observations Spatiales (LATMOS) Sorbonne Université (SU)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS) 2018 https://hal-insu.archives-ouvertes.fr/insu-01808641 https://hal-insu.archives-ouvertes.fr/insu-01808641/document https://hal-insu.archives-ouvertes.fr/insu-01808641/file/acp-18-13075-2018.pdf https://doi.org/10.5194/acp-18-13075-2018 en eng HAL CCSD European Geosciences Union info:eu-repo/semantics/altIdentifier/doi/10.5194/acp-18-13075-2018 insu-01808641 https://hal-insu.archives-ouvertes.fr/insu-01808641 https://hal-insu.archives-ouvertes.fr/insu-01808641/document https://hal-insu.archives-ouvertes.fr/insu-01808641/file/acp-18-13075-2018.pdf doi:10.5194/acp-18-13075-2018 info:eu-repo/semantics/OpenAccess ISSN: 1680-7316 EISSN: 1680-7324 Atmospheric Chemistry and Physics https://hal-insu.archives-ouvertes.fr/insu-01808641 Atmospheric Chemistry and Physics, European Geosciences Union, 2018, 18, pp.13075-13095. ⟨10.5194/acp-18-13075-2018⟩ [PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph] info:eu-repo/semantics/article Journal articles 2018 ftccsdartic https://doi.org/10.5194/acp-18-13075-2018 2021-12-19T00:55:41Z International audience To investigate the origin of springtime aerosols in the Arctic region we performed ground-based and airborne 355nm Raman lidar observations in the north of Norway (Hammerfest). Two lidars were embedded (i) on an ultralight aircraft for vertical (nadir) or horizontal line-of-sight measurements and (ii) in an air-conditioned van on the ground for vertical (zenith) measurements. This field experiment was designed as part of the Pollution in the ARCtic System (PARCS) project of the French Arctic Initiative and took place from 13 to 26 May 2016. The consistency among lidar measurements is verified by comparing nadir, horizontal line of sight, and ground-based Raman lidar profiles. Dispersion of the order of 0.01km −1 is obtained among lidar-derived aerosol extinction coefficients at 355nm. The aerosol load measured in the first 3km of the troposphere remains low throughout the campaign, with aerosol optical thickness (AOT) of 0.1 at 355nm ( ∼ 0.05 at 550nm). The main contributors to the evolution of the aerosol load at low altitude prove to be one of the flares of the nearby Melkøya gas processing facility, the oceanic source, and the transport of aerosols from industrial sites in Russia. Moreover, ground-based lidar measurements allowed us to identify three cases of long-range aerosol transport (between 3 and 8km above the mean sea level). Using back trajectories computed with the Lagrangian model FLEXPART-WRF, these aerosol plumes are shown to be the result of the strong forest fires that occurred in the area of Fort McMurray, in Canada. They can at most double the AOT value over the Arctic area, with an anomaly of 0.1 on the AOT at 355nm. Article in Journal/Newspaper Arctic Fort McMurray Hammerfest Northern Norway Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) Arctic Fort McMurray Canada Norway Atmospheric Chemistry and Physics 18 17 13075 13095