Vertical aerosol distribution in the southern hemispheric midlatitudes as observed with lidar in Punta Arenas, Chile (53.2° and 70.9° W), during ALPACA

Within this publication, lidar observations of the vertical aerosol distribution above Punta Arenas, Chile (53.2 S and 70.9 W), which have been performed with the Raman lidar PollyXT from December 2009 to April 2010, are presented. Pristine marine aerosol conditions related to the prevailing westerl...

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Main Authors: Foth, Andreas, Kanitz, Thomas, Engelmann, Ronny, Baars, Holger, Radenz, Martin, Seifert, Patric, Barja, Boris, Fromm, Michael, Kalesse, Heike, Ansmann, Albert
Format: Article in Journal/Newspaper
Language:English
Published: Katlenburg-Lindau : EGU 2019
Subjects:
550
Online Access:https://oa.tib.eu/renate/handle/123456789/6950
https://doi.org/10.34657/5997
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spelling ftleibnizopen:oai:oai.leibnizopen.de:uTiJYIgBdbrxVwz6gVi8 2023-06-11T04:03:03+02:00 Vertical aerosol distribution in the southern hemispheric midlatitudes as observed with lidar in Punta Arenas, Chile (53.2° and 70.9° W), during ALPACA Foth, Andreas Kanitz, Thomas Engelmann, Ronny Baars, Holger Radenz, Martin Seifert, Patric Barja, Boris Fromm, Michael Kalesse, Heike Ansmann, Albert 2019 application/pdf https://oa.tib.eu/renate/handle/123456789/6950 https://doi.org/10.34657/5997 eng eng Katlenburg-Lindau : EGU CC BY 4.0 Unported https://creativecommons.org/licenses/by/4.0/ Atmospheric chemistry and physics 19 (2019), Nr. 9 AERONET aerosol biomass burning boundary layer CALIOP CALIPSO lidar long range transport optical property photometer Raman spectroscopy troposphere Australia Chile Magallanes Patagonia Punta Arenas 550 article Text 2019 ftleibnizopen https://doi.org/10.34657/5997 2023-05-28T23:28:40Z Within this publication, lidar observations of the vertical aerosol distribution above Punta Arenas, Chile (53.2 S and 70.9 W), which have been performed with the Raman lidar PollyXT from December 2009 to April 2010, are presented. Pristine marine aerosol conditions related to the prevailing westerly circulation dominated the measurements. Lofted aerosol layers could only be observed eight times during the whole measurement period. Two case studies are presented showing long-range transport of smoke from biomass burning in Australia and regionally transported dust from the Patagonian Desert, respectively. The aerosol sources are identified by trajectory analyses with the Hybrid Single-Particle Lagrangian Integrated Trajectory (HYSPLIT) and FLEXible PARTicle dispersion model (FLEXPART). However, seven of the eight analysed cases with lofted layers show an aerosol optical thickness of less than 0.05. From the lidar observations, a mean planetary boundary layer (PBL) top height of 1150 350m was determined. An analysis of particle backscatter coefficients confirms that the majority of the aerosol is attributed to the PBL, while the free troposphere is characterized by a very low background aerosol concentration. The ground-based lidar observations at 532 and 1064 nm are supplemented by the Aerosol Robotic Network (AERONET) Sun photometers and the space-borne Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP) aboard the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation (CALIPSO). The averaged aerosol optical thickness (AOT) determined by CALIOP was 0:02 0:01 in Punta Arenas from 2009 to 2010. © Author(s) 2019. This work is distributed under the Creative Commons Attribution 4.0 License. publishedVersion Article in Journal/Newspaper Aerosol Robotic Network LeibnizOpen (The Leibniz Association) Magallanes ENVELOPE(-62.933,-62.933,-64.883,-64.883) Patagonia
institution Open Polar
collection LeibnizOpen (The Leibniz Association)
op_collection_id ftleibnizopen
language English
topic AERONET
aerosol
biomass burning
boundary layer
CALIOP
CALIPSO
lidar
long range transport
optical property
photometer
Raman spectroscopy
troposphere
Australia
Chile
Magallanes
Patagonia
Punta Arenas
550
spellingShingle AERONET
aerosol
biomass burning
boundary layer
CALIOP
CALIPSO
lidar
long range transport
optical property
photometer
Raman spectroscopy
troposphere
Australia
Chile
Magallanes
Patagonia
Punta Arenas
550
Foth, Andreas
Kanitz, Thomas
Engelmann, Ronny
Baars, Holger
Radenz, Martin
Seifert, Patric
Barja, Boris
Fromm, Michael
Kalesse, Heike
Ansmann, Albert
Vertical aerosol distribution in the southern hemispheric midlatitudes as observed with lidar in Punta Arenas, Chile (53.2° and 70.9° W), during ALPACA
topic_facet AERONET
aerosol
biomass burning
boundary layer
CALIOP
CALIPSO
lidar
long range transport
optical property
photometer
Raman spectroscopy
troposphere
Australia
Chile
Magallanes
Patagonia
Punta Arenas
550
description Within this publication, lidar observations of the vertical aerosol distribution above Punta Arenas, Chile (53.2 S and 70.9 W), which have been performed with the Raman lidar PollyXT from December 2009 to April 2010, are presented. Pristine marine aerosol conditions related to the prevailing westerly circulation dominated the measurements. Lofted aerosol layers could only be observed eight times during the whole measurement period. Two case studies are presented showing long-range transport of smoke from biomass burning in Australia and regionally transported dust from the Patagonian Desert, respectively. The aerosol sources are identified by trajectory analyses with the Hybrid Single-Particle Lagrangian Integrated Trajectory (HYSPLIT) and FLEXible PARTicle dispersion model (FLEXPART). However, seven of the eight analysed cases with lofted layers show an aerosol optical thickness of less than 0.05. From the lidar observations, a mean planetary boundary layer (PBL) top height of 1150 350m was determined. An analysis of particle backscatter coefficients confirms that the majority of the aerosol is attributed to the PBL, while the free troposphere is characterized by a very low background aerosol concentration. The ground-based lidar observations at 532 and 1064 nm are supplemented by the Aerosol Robotic Network (AERONET) Sun photometers and the space-borne Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP) aboard the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation (CALIPSO). The averaged aerosol optical thickness (AOT) determined by CALIOP was 0:02 0:01 in Punta Arenas from 2009 to 2010. © Author(s) 2019. This work is distributed under the Creative Commons Attribution 4.0 License. publishedVersion
format Article in Journal/Newspaper
author Foth, Andreas
Kanitz, Thomas
Engelmann, Ronny
Baars, Holger
Radenz, Martin
Seifert, Patric
Barja, Boris
Fromm, Michael
Kalesse, Heike
Ansmann, Albert
author_facet Foth, Andreas
Kanitz, Thomas
Engelmann, Ronny
Baars, Holger
Radenz, Martin
Seifert, Patric
Barja, Boris
Fromm, Michael
Kalesse, Heike
Ansmann, Albert
author_sort Foth, Andreas
title Vertical aerosol distribution in the southern hemispheric midlatitudes as observed with lidar in Punta Arenas, Chile (53.2° and 70.9° W), during ALPACA
title_short Vertical aerosol distribution in the southern hemispheric midlatitudes as observed with lidar in Punta Arenas, Chile (53.2° and 70.9° W), during ALPACA
title_full Vertical aerosol distribution in the southern hemispheric midlatitudes as observed with lidar in Punta Arenas, Chile (53.2° and 70.9° W), during ALPACA
title_fullStr Vertical aerosol distribution in the southern hemispheric midlatitudes as observed with lidar in Punta Arenas, Chile (53.2° and 70.9° W), during ALPACA
title_full_unstemmed Vertical aerosol distribution in the southern hemispheric midlatitudes as observed with lidar in Punta Arenas, Chile (53.2° and 70.9° W), during ALPACA
title_sort vertical aerosol distribution in the southern hemispheric midlatitudes as observed with lidar in punta arenas, chile (53.2° and 70.9° w), during alpaca
publisher Katlenburg-Lindau : EGU
publishDate 2019
url https://oa.tib.eu/renate/handle/123456789/6950
https://doi.org/10.34657/5997
long_lat ENVELOPE(-62.933,-62.933,-64.883,-64.883)
geographic Magallanes
Patagonia
geographic_facet Magallanes
Patagonia
genre Aerosol Robotic Network
genre_facet Aerosol Robotic Network
op_source Atmospheric chemistry and physics 19 (2019), Nr. 9
op_rights CC BY 4.0 Unported
https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.34657/5997
_version_ 1768371540009680896