MAX-DOAS measurements of atmospheric trace gases in Ny-Ålesund - Radiative transfer studies and their application

A new approach to derive tropospheric concentrations of some atmospheric trace gases from ground-based UV/vis measurements is described. The instrument, referred to as the MAX-DOAS, is based on the well-known UV/vis instruments, which use the sunlight scattered in the zenith sky as the light source...

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Main Authors: F. Wittrock, H. Oetjen, A. Richter, S. Fietkau, T. Medeke, A. Rozanov, J. P. Burrows
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2004
Subjects:
Online Access:https://doaj.org/article/d72101fb483d4315bd028248d85da2e9
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spelling ftdoajarticles:oai:doaj.org/article:d72101fb483d4315bd028248d85da2e9 2023-05-15T17:48:23+02:00 MAX-DOAS measurements of atmospheric trace gases in Ny-Ålesund - Radiative transfer studies and their application F. Wittrock H. Oetjen A. Richter S. Fietkau T. Medeke A. Rozanov J. P. Burrows 2004-01-01T00:00:00Z https://doaj.org/article/d72101fb483d4315bd028248d85da2e9 EN eng Copernicus Publications http://www.atmos-chem-phys.net/4/955/2004/acp-4-955-2004.pdf https://doaj.org/toc/1680-7316 https://doaj.org/toc/1680-7324 1680-7316 1680-7324 https://doaj.org/article/d72101fb483d4315bd028248d85da2e9 Atmospheric Chemistry and Physics, Vol 4, Iss 4, Pp 955-966 (2004) Physics QC1-999 Chemistry QD1-999 article 2004 ftdoajarticles 2022-12-31T11:29:18Z A new approach to derive tropospheric concentrations of some atmospheric trace gases from ground-based UV/vis measurements is described. The instrument, referred to as the MAX-DOAS, is based on the well-known UV/vis instruments, which use the sunlight scattered in the zenith sky as the light source and the method of Differential Optical Absorption Spectroscopy (DOAS) to derive column amounts of absorbers like ozone and nitrogen dioxide. Substantial enhancements have been applied to this standard setup to use different lines of sight near to the horizon as additional light sources (MAX - multi axis). Results from measurements at Ny-Ålesund (79° N, 12° E) are presented and interpreted with the full-spherical radiative transfer model SCIATRAN. In particular, measurements of the oxygen dimer O 4 which has a known column and vertical distribution in the atmosphere are used to evaluate the sensitivity of the retrieval to parameters such as multiple scattering, solar azimuth, surface albedo and refraction in the atmosphere and also to validate the radiative transfer model. As a first application, measurements of NO 2 emissions from a ship lying in Ny-Ålesund harbour are presented. The results of this study demonstrate the feasibility of long term UV/vis multi axis measurement that can be used to derive not only column amounts of different trace gases but also some information on the vertical location of these absorbers. Article in Journal/Newspaper Ny Ålesund Ny-Ålesund Directory of Open Access Journals: DOAJ Articles Ny-Ålesund
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Physics
QC1-999
Chemistry
QD1-999
spellingShingle Physics
QC1-999
Chemistry
QD1-999
F. Wittrock
H. Oetjen
A. Richter
S. Fietkau
T. Medeke
A. Rozanov
J. P. Burrows
MAX-DOAS measurements of atmospheric trace gases in Ny-Ålesund - Radiative transfer studies and their application
topic_facet Physics
QC1-999
Chemistry
QD1-999
description A new approach to derive tropospheric concentrations of some atmospheric trace gases from ground-based UV/vis measurements is described. The instrument, referred to as the MAX-DOAS, is based on the well-known UV/vis instruments, which use the sunlight scattered in the zenith sky as the light source and the method of Differential Optical Absorption Spectroscopy (DOAS) to derive column amounts of absorbers like ozone and nitrogen dioxide. Substantial enhancements have been applied to this standard setup to use different lines of sight near to the horizon as additional light sources (MAX - multi axis). Results from measurements at Ny-Ålesund (79° N, 12° E) are presented and interpreted with the full-spherical radiative transfer model SCIATRAN. In particular, measurements of the oxygen dimer O 4 which has a known column and vertical distribution in the atmosphere are used to evaluate the sensitivity of the retrieval to parameters such as multiple scattering, solar azimuth, surface albedo and refraction in the atmosphere and also to validate the radiative transfer model. As a first application, measurements of NO 2 emissions from a ship lying in Ny-Ålesund harbour are presented. The results of this study demonstrate the feasibility of long term UV/vis multi axis measurement that can be used to derive not only column amounts of different trace gases but also some information on the vertical location of these absorbers.
format Article in Journal/Newspaper
author F. Wittrock
H. Oetjen
A. Richter
S. Fietkau
T. Medeke
A. Rozanov
J. P. Burrows
author_facet F. Wittrock
H. Oetjen
A. Richter
S. Fietkau
T. Medeke
A. Rozanov
J. P. Burrows
author_sort F. Wittrock
title MAX-DOAS measurements of atmospheric trace gases in Ny-Ålesund - Radiative transfer studies and their application
title_short MAX-DOAS measurements of atmospheric trace gases in Ny-Ålesund - Radiative transfer studies and their application
title_full MAX-DOAS measurements of atmospheric trace gases in Ny-Ålesund - Radiative transfer studies and their application
title_fullStr MAX-DOAS measurements of atmospheric trace gases in Ny-Ålesund - Radiative transfer studies and their application
title_full_unstemmed MAX-DOAS measurements of atmospheric trace gases in Ny-Ålesund - Radiative transfer studies and their application
title_sort max-doas measurements of atmospheric trace gases in ny-ålesund - radiative transfer studies and their application
publisher Copernicus Publications
publishDate 2004
url https://doaj.org/article/d72101fb483d4315bd028248d85da2e9
geographic Ny-Ålesund
geographic_facet Ny-Ålesund
genre Ny Ålesund
Ny-Ålesund
genre_facet Ny Ålesund
Ny-Ålesund
op_source Atmospheric Chemistry and Physics, Vol 4, Iss 4, Pp 955-966 (2004)
op_relation http://www.atmos-chem-phys.net/4/955/2004/acp-4-955-2004.pdf
https://doaj.org/toc/1680-7316
https://doaj.org/toc/1680-7324
1680-7316
1680-7324
https://doaj.org/article/d72101fb483d4315bd028248d85da2e9
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