Odin stratospheric proxy NO<sub>y</sub> measurements and climatology

Five years of OSIRIS (Optical Spectrograph and InfraRed Imager System) NO<sub>2</sub> and SMR (Sub-millimetre and Millimetre Radiometer) HNO<sub>3</sub> observations from the Odin satellite, combined with data from a photochemical box model, have been used to construct a stra...

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Main Authors: D. Murtagh, A. I. Jonsson, C. S. Haley, J. Urban, C. A. McLinden, S. Brohede
Format: Article
Language:English
Published: Copernicus Publications 2008-10-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/8/5731/2008/acp-8-5731-2008.pdf
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spelling doaj-a6356cc98b79498fbd176929e2cd0a162020-11-25T00:09:17ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242008-10-0181957315754Odin stratospheric proxy NO<sub>y</sub> measurements and climatologyD. MurtaghA. I. JonssonC. S. HaleyJ. UrbanC. A. McLindenS. BrohedeFive years of OSIRIS (Optical Spectrograph and InfraRed Imager System) NO<sub>2</sub> and SMR (Sub-millimetre and Millimetre Radiometer) HNO<sub>3</sub> observations from the Odin satellite, combined with data from a photochemical box model, have been used to construct a stratospheric proxy NO<sub>y</sub> data set including the gases: NO, NO<sub>2</sub>, HNO<sub>3</sub>, 2&times;N<sub>2</sub>O<sub>5</sub> and ClONO<sub>2</sub>. This Odin NO<sub>y</sub> climatology is based on all daytime measurements and contains monthly mean and standard deviation, expressed as mixing ratio or number density, as function of latitude or equivalent latitude (5&deg; bins) on 17 vertical layers (altitude, pressure or potential temperature) between 14 and 46 km. Comparisons with coincident NO<sub>y</sub> profiles from the Atmospheric Chemistry Experiment-Fourier Transform Spectrometer (ACE-FTS) instrument were used to evaluate several methods to combine Odin observations with model data. This comparison indicates that the most appropriate merging technique uses OSIRIS measurements of NO<sub>2</sub>, scaled with model NO/NO<sub>2</sub> ratios, to estimate NO. The sum of 2&times;N<sub>2</sub>O<sub>5</sub> and ClONO<sub>2</sub> is estimated from uncertainty-based weighted averages of scaled observations of SMR HNO<sub>3</sub> and OSIRIS NO<sub>2</sub>. Comparisons with ACE-FTS suggest the precision (random error) and accuracy (systematic error) of Odin NO<sub>y</sub> profiles are about 15% and 20%, respectively. Further comparisons between Odin and the Canadian Middle Atmosphere Model (CMAM) show agreement to within 20% and 2 ppb throughout most of the stratosphere except in the polar vortices. The combination of good temporal and spatial coverage, a relatively long data record, and good accuracy and precision make this a valuable NO<sub>y</sub> product for various atmospheric studies and model assessments. http://www.atmos-chem-phys.net/8/5731/2008/acp-8-5731-2008.pdf
collection DOAJ
language English
format Article
sources DOAJ
author D. Murtagh
A. I. Jonsson
C. S. Haley
J. Urban
C. A. McLinden
S. Brohede
spellingShingle D. Murtagh
A. I. Jonsson
C. S. Haley
J. Urban
C. A. McLinden
S. Brohede
Odin stratospheric proxy NO<sub>y</sub> measurements and climatology
Atmospheric Chemistry and Physics
author_facet D. Murtagh
A. I. Jonsson
C. S. Haley
J. Urban
C. A. McLinden
S. Brohede
author_sort D. Murtagh
title Odin stratospheric proxy NO<sub>y</sub> measurements and climatology
title_short Odin stratospheric proxy NO<sub>y</sub> measurements and climatology
title_full Odin stratospheric proxy NO<sub>y</sub> measurements and climatology
title_fullStr Odin stratospheric proxy NO<sub>y</sub> measurements and climatology
title_full_unstemmed Odin stratospheric proxy NO<sub>y</sub> measurements and climatology
title_sort odin stratospheric proxy no<sub>y</sub> measurements and climatology
publisher Copernicus Publications
series Atmospheric Chemistry and Physics
issn 1680-7316
1680-7324
publishDate 2008-10-01
description Five years of OSIRIS (Optical Spectrograph and InfraRed Imager System) NO<sub>2</sub> and SMR (Sub-millimetre and Millimetre Radiometer) HNO<sub>3</sub> observations from the Odin satellite, combined with data from a photochemical box model, have been used to construct a stratospheric proxy NO<sub>y</sub> data set including the gases: NO, NO<sub>2</sub>, HNO<sub>3</sub>, 2&times;N<sub>2</sub>O<sub>5</sub> and ClONO<sub>2</sub>. This Odin NO<sub>y</sub> climatology is based on all daytime measurements and contains monthly mean and standard deviation, expressed as mixing ratio or number density, as function of latitude or equivalent latitude (5&deg; bins) on 17 vertical layers (altitude, pressure or potential temperature) between 14 and 46 km. Comparisons with coincident NO<sub>y</sub> profiles from the Atmospheric Chemistry Experiment-Fourier Transform Spectrometer (ACE-FTS) instrument were used to evaluate several methods to combine Odin observations with model data. This comparison indicates that the most appropriate merging technique uses OSIRIS measurements of NO<sub>2</sub>, scaled with model NO/NO<sub>2</sub> ratios, to estimate NO. The sum of 2&times;N<sub>2</sub>O<sub>5</sub> and ClONO<sub>2</sub> is estimated from uncertainty-based weighted averages of scaled observations of SMR HNO<sub>3</sub> and OSIRIS NO<sub>2</sub>. Comparisons with ACE-FTS suggest the precision (random error) and accuracy (systematic error) of Odin NO<sub>y</sub> profiles are about 15% and 20%, respectively. Further comparisons between Odin and the Canadian Middle Atmosphere Model (CMAM) show agreement to within 20% and 2 ppb throughout most of the stratosphere except in the polar vortices. The combination of good temporal and spatial coverage, a relatively long data record, and good accuracy and precision make this a valuable NO<sub>y</sub> product for various atmospheric studies and model assessments.
url http://www.atmos-chem-phys.net/8/5731/2008/acp-8-5731-2008.pdf
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