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...
Published in: | Atmospheric Chemistry and Physics |
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Main Authors: | , , |
Other Authors: | , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
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HAL CCSD
2018
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Online Access: | https://insu.hal.science/insu-01808641 https://insu.hal.science/insu-01808641/document https://insu.hal.science/insu-01808641/file/acp-18-13075-2018.pdf https://doi.org/10.5194/acp-18-13075-2018 |
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ftceafr:oai:HAL:insu-01808641v1 |
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institution |
Open Polar |
collection |
HAL-CEA (Commissariat à l'énergie atomique et aux énergies alternatives) |
op_collection_id |
ftceafr |
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) 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)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)) Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA) Chimie Atmosphérique Expérimentale (CAE) Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-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)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)) TROPO - LATMOS Laboratoire Atmosphères, Milieux, Observations Spatiales (LATMOS) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (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://insu.hal.science/insu-01808641 https://insu.hal.science/insu-01808641/document https://insu.hal.science/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://insu.hal.science/insu-01808641 Atmospheric Chemistry and Physics, 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://insu.hal.science/insu-01808641 https://insu.hal.science/insu-01808641/document https://insu.hal.science/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 |
_version_ |
1801372369835524096 |
spelling |
ftceafr:oai:HAL:insu-01808641v1 2024-06-09T07:43:33+00:00 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) 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)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)) Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA) Chimie Atmosphérique Expérimentale (CAE) Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-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)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)) TROPO - LATMOS Laboratoire Atmosphères, Milieux, Observations Spatiales (LATMOS) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS) 2018 https://insu.hal.science/insu-01808641 https://insu.hal.science/insu-01808641/document https://insu.hal.science/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://insu.hal.science/insu-01808641 https://insu.hal.science/insu-01808641/document https://insu.hal.science/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://insu.hal.science/insu-01808641 Atmospheric Chemistry and Physics, 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 ftceafr https://doi.org/10.5194/acp-18-13075-2018 2024-05-16T14:51:36Z 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 HAL-CEA (Commissariat à l'énergie atomique et aux énergies alternatives) Arctic Fort McMurray Canada Norway Atmospheric Chemistry and Physics 18 17 13075 13095 |