Year-round stratospheric aerosol backscatter ratios calculated from lidar measurements above northern Norway

We present a new method for calculating backscatter ratios of the stratospheric sulfate aerosol (SSA) layer from daytime and nighttime lidar measurements. Using this new method we show a first year-round dataset of stratospheric aerosol backscatter ratios at high latitudes. The SSA layer is located...

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Published in:Atmospheric Measurement Techniques
Main Authors: Langenbach, Arvid, Baumgarten, Gerd, Fiedler, Jens, Lübken, Franz-Josef, Savigny, Christian, Zalach, Jacob
Format: Text
Language:English
Published: 2019
Subjects:
Online Access:https://doi.org/10.5194/amt-12-4065-2019
https://amt.copernicus.org/articles/12/4065/2019/
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spelling ftcopernicus:oai:publications.copernicus.org:amt74638 2023-05-15T15:11:09+02:00 Year-round stratospheric aerosol backscatter ratios calculated from lidar measurements above northern Norway Langenbach, Arvid Baumgarten, Gerd Fiedler, Jens Lübken, Franz-Josef Savigny, Christian Zalach, Jacob 2019-07-24 application/pdf https://doi.org/10.5194/amt-12-4065-2019 https://amt.copernicus.org/articles/12/4065/2019/ eng eng doi:10.5194/amt-12-4065-2019 https://amt.copernicus.org/articles/12/4065/2019/ eISSN: 1867-8548 Text 2019 ftcopernicus https://doi.org/10.5194/amt-12-4065-2019 2020-07-20T16:22:44Z We present a new method for calculating backscatter ratios of the stratospheric sulfate aerosol (SSA) layer from daytime and nighttime lidar measurements. Using this new method we show a first year-round dataset of stratospheric aerosol backscatter ratios at high latitudes. The SSA layer is located at altitudes between the tropopause and about 30 km. It is of fundamental importance for the radiative balance of the atmosphere. We use a state-of-the-art Rayleigh–Mie–Raman lidar at the Arctic Lidar Observatory for Middle Atmosphere Research (ALOMAR) station located in northern Norway (69 ∘ N, 16 ∘ E; 380 m a.s.l.). For nighttime measurements the aerosol backscatter ratios are derived using elastic and inelastic backscatter of the emitted laser wavelengths 355, 532 and 1064 nm . The setup of the lidar allows measurements with a resolution of about 5 min in time and 150 m in altitude to be performed in high quality, which enables the identification of multiple sub-layers in the stratospheric aerosol layer of less than 1 km vertical thickness. We introduce a method to extend the dataset throughout the summer when measurements need to be performed under permanent daytime conditions. For that purpose we approximate the backscatter ratios from color ratios of elastic scattering and apply a correction function. We calculate the correction function using the average backscatter ratio profile at 355 nm from about 1700 h of nighttime measurements from the years 2000 to 2018. Using the new method we finally present a year-round dataset based on about 4100 h of measurements during the years 2014 to 2017. Text Arctic Northern Norway Copernicus Publications: E-Journals Alomar ENVELOPE(-67.083,-67.083,-68.133,-68.133) Arctic Norway Atmospheric Measurement Techniques 12 7 4065 4076
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description We present a new method for calculating backscatter ratios of the stratospheric sulfate aerosol (SSA) layer from daytime and nighttime lidar measurements. Using this new method we show a first year-round dataset of stratospheric aerosol backscatter ratios at high latitudes. The SSA layer is located at altitudes between the tropopause and about 30 km. It is of fundamental importance for the radiative balance of the atmosphere. We use a state-of-the-art Rayleigh–Mie–Raman lidar at the Arctic Lidar Observatory for Middle Atmosphere Research (ALOMAR) station located in northern Norway (69 ∘ N, 16 ∘ E; 380 m a.s.l.). For nighttime measurements the aerosol backscatter ratios are derived using elastic and inelastic backscatter of the emitted laser wavelengths 355, 532 and 1064 nm . The setup of the lidar allows measurements with a resolution of about 5 min in time and 150 m in altitude to be performed in high quality, which enables the identification of multiple sub-layers in the stratospheric aerosol layer of less than 1 km vertical thickness. We introduce a method to extend the dataset throughout the summer when measurements need to be performed under permanent daytime conditions. For that purpose we approximate the backscatter ratios from color ratios of elastic scattering and apply a correction function. We calculate the correction function using the average backscatter ratio profile at 355 nm from about 1700 h of nighttime measurements from the years 2000 to 2018. Using the new method we finally present a year-round dataset based on about 4100 h of measurements during the years 2014 to 2017.
format Text
author Langenbach, Arvid
Baumgarten, Gerd
Fiedler, Jens
Lübken, Franz-Josef
Savigny, Christian
Zalach, Jacob
spellingShingle Langenbach, Arvid
Baumgarten, Gerd
Fiedler, Jens
Lübken, Franz-Josef
Savigny, Christian
Zalach, Jacob
Year-round stratospheric aerosol backscatter ratios calculated from lidar measurements above northern Norway
author_facet Langenbach, Arvid
Baumgarten, Gerd
Fiedler, Jens
Lübken, Franz-Josef
Savigny, Christian
Zalach, Jacob
author_sort Langenbach, Arvid
title Year-round stratospheric aerosol backscatter ratios calculated from lidar measurements above northern Norway
title_short Year-round stratospheric aerosol backscatter ratios calculated from lidar measurements above northern Norway
title_full Year-round stratospheric aerosol backscatter ratios calculated from lidar measurements above northern Norway
title_fullStr Year-round stratospheric aerosol backscatter ratios calculated from lidar measurements above northern Norway
title_full_unstemmed Year-round stratospheric aerosol backscatter ratios calculated from lidar measurements above northern Norway
title_sort year-round stratospheric aerosol backscatter ratios calculated from lidar measurements above northern norway
publishDate 2019
url https://doi.org/10.5194/amt-12-4065-2019
https://amt.copernicus.org/articles/12/4065/2019/
long_lat ENVELOPE(-67.083,-67.083,-68.133,-68.133)
geographic Alomar
Arctic
Norway
geographic_facet Alomar
Arctic
Norway
genre Arctic
Northern Norway
genre_facet Arctic
Northern Norway
op_source eISSN: 1867-8548
op_relation doi:10.5194/amt-12-4065-2019
https://amt.copernicus.org/articles/12/4065/2019/
op_doi https://doi.org/10.5194/amt-12-4065-2019
container_title Atmospheric Measurement Techniques
container_volume 12
container_issue 7
container_start_page 4065
op_container_end_page 4076
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