Saharan dust long-range transport across the Atlantic studied by an airborne Doppler wind lidar and the MACC model

A huge amount of dust is transported every year from north Africa into the Caribbean region. This paper presents an investigation of this long-range transport process based on airborne Doppler wind lidar (DWL) measurements conducted during the SALTRACE campaign (June–July 2013), as well as an evalua...

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Published in:Atmospheric Chemistry and Physics
Main Authors: Chouza, Fernando, Reitebuch, Oliver, Benedetti, Angela, Weinzierl, Bernadett
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/acp-16-11581-2016
https://www.atmos-chem-phys.net/16/11581/2016/
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spelling ftcopernicus:oai:publications.copernicus.org:acp51195 2023-05-15T17:35:16+02:00 Saharan dust long-range transport across the Atlantic studied by an airborne Doppler wind lidar and the MACC model Chouza, Fernando Reitebuch, Oliver Benedetti, Angela Weinzierl, Bernadett 2018-09-12 application/pdf https://doi.org/10.5194/acp-16-11581-2016 https://www.atmos-chem-phys.net/16/11581/2016/ eng eng doi:10.5194/acp-16-11581-2016 https://www.atmos-chem-phys.net/16/11581/2016/ eISSN: 1680-7324 Text 2018 ftcopernicus https://doi.org/10.5194/acp-16-11581-2016 2019-12-24T09:51:59Z A huge amount of dust is transported every year from north Africa into the Caribbean region. This paper presents an investigation of this long-range transport process based on airborne Doppler wind lidar (DWL) measurements conducted during the SALTRACE campaign (June–July 2013), as well as an evaluation of the ability of the MACC (Monitoring Atmospheric Composition and Climate) global aerosol model to reproduce it and its associated features. Although both the modeled winds from MACC and the measurements from the DWL show a generally good agreement, some differences, particularly in the African easterly jet (AEJ) intensity, were noted. The observed differences between modeled and measured wind jet speeds are between 5 and 10 m s −1 . The vertical aerosol distribution within the Saharan dust plume and the marine boundary layer is investigated during the June–July 2013 period based on the MACC aerosol model results and the CALIOP satellite lidar measurements. While the modeled Saharan dust plume extent shows a good agreement with the measurements, a systematic underestimation of the marine boundary layer extinction is observed. Additionally, three selected case studies covering different aspects of the Saharan dust long-range transport along the west African coast, over the North Atlantic Ocean and the Caribbean are presented. For the first time, DWL measurements are used to investigate the Saharan dust long-range transport. Simultaneous wind and backscatter measurements from the DWL are used, in combination with the MACC model, to analyze different features associated with the long-range transport, including an African easterly wave trough, the AEJ and the intertropical convergence zone. Text North Atlantic Copernicus Publications: E-Journals Atmospheric Chemistry and Physics 16 18 11581 11600
institution Open Polar
collection Copernicus Publications: E-Journals
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language English
description A huge amount of dust is transported every year from north Africa into the Caribbean region. This paper presents an investigation of this long-range transport process based on airborne Doppler wind lidar (DWL) measurements conducted during the SALTRACE campaign (June–July 2013), as well as an evaluation of the ability of the MACC (Monitoring Atmospheric Composition and Climate) global aerosol model to reproduce it and its associated features. Although both the modeled winds from MACC and the measurements from the DWL show a generally good agreement, some differences, particularly in the African easterly jet (AEJ) intensity, were noted. The observed differences between modeled and measured wind jet speeds are between 5 and 10 m s −1 . The vertical aerosol distribution within the Saharan dust plume and the marine boundary layer is investigated during the June–July 2013 period based on the MACC aerosol model results and the CALIOP satellite lidar measurements. While the modeled Saharan dust plume extent shows a good agreement with the measurements, a systematic underestimation of the marine boundary layer extinction is observed. Additionally, three selected case studies covering different aspects of the Saharan dust long-range transport along the west African coast, over the North Atlantic Ocean and the Caribbean are presented. For the first time, DWL measurements are used to investigate the Saharan dust long-range transport. Simultaneous wind and backscatter measurements from the DWL are used, in combination with the MACC model, to analyze different features associated with the long-range transport, including an African easterly wave trough, the AEJ and the intertropical convergence zone.
format Text
author Chouza, Fernando
Reitebuch, Oliver
Benedetti, Angela
Weinzierl, Bernadett
spellingShingle Chouza, Fernando
Reitebuch, Oliver
Benedetti, Angela
Weinzierl, Bernadett
Saharan dust long-range transport across the Atlantic studied by an airborne Doppler wind lidar and the MACC model
author_facet Chouza, Fernando
Reitebuch, Oliver
Benedetti, Angela
Weinzierl, Bernadett
author_sort Chouza, Fernando
title Saharan dust long-range transport across the Atlantic studied by an airborne Doppler wind lidar and the MACC model
title_short Saharan dust long-range transport across the Atlantic studied by an airborne Doppler wind lidar and the MACC model
title_full Saharan dust long-range transport across the Atlantic studied by an airborne Doppler wind lidar and the MACC model
title_fullStr Saharan dust long-range transport across the Atlantic studied by an airborne Doppler wind lidar and the MACC model
title_full_unstemmed Saharan dust long-range transport across the Atlantic studied by an airborne Doppler wind lidar and the MACC model
title_sort saharan dust long-range transport across the atlantic studied by an airborne doppler wind lidar and the macc model
publishDate 2018
url https://doi.org/10.5194/acp-16-11581-2016
https://www.atmos-chem-phys.net/16/11581/2016/
genre North Atlantic
genre_facet North Atlantic
op_source eISSN: 1680-7324
op_relation doi:10.5194/acp-16-11581-2016
https://www.atmos-chem-phys.net/16/11581/2016/
op_doi https://doi.org/10.5194/acp-16-11581-2016
container_title Atmospheric Chemistry and Physics
container_volume 16
container_issue 18
container_start_page 11581
op_container_end_page 11600
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