Measurements of CH<sub>3</sub>O<sub>2</sub>NO<sub>2</sub> in the upper troposphere

Methyl peroxy nitrate (CH<sub>3</sub>O<sub>2</sub>NO<sub>2</sub>) is a non-acyl peroxy nitrate that is important for photochemistry at low temperatures characteristic of the upper troposphere. We report the first measurements of CH<sub>3</sub>O<sub&...

Full description

Bibliographic Details
Main Authors: B. A. Nault, C. Garland, S. E. Pusede, P. J. Wooldridge, K. Ullmann, S. R. Hall, R. C. Cohen
Format: Article
Language:English
Published: Copernicus Publications 2015-02-01
Series:Atmospheric Measurement Techniques
Online Access:http://www.atmos-meas-tech.net/8/987/2015/amt-8-987-2015.pdf
id doaj-122257e8fcc84cf398093900a14b4a6a
record_format Article
spelling doaj-122257e8fcc84cf398093900a14b4a6a2020-11-25T00:24:56ZengCopernicus PublicationsAtmospheric Measurement Techniques1867-13811867-85482015-02-018298799710.5194/amt-8-987-2015Measurements of CH<sub>3</sub>O<sub>2</sub>NO<sub>2</sub> in the upper troposphereB. A. Nault0C. Garland1S. E. Pusede2P. J. Wooldridge3K. Ullmann4S. R. Hall5R. C. Cohen6Department of Earth and Planetary Science, University of California at Berkeley, Berkeley, CA, USADepartment of Chemistry, University of California at Berkeley, Berkeley, CA, USADepartment of Chemistry, University of California at Berkeley, Berkeley, CA, USADepartment of Chemistry, University of California at Berkeley, Berkeley, CA, USAAtmospheric Chemistry Division, National Center for Atmospheric Research, Boulder, CO, USAAtmospheric Chemistry Division, National Center for Atmospheric Research, Boulder, CO, USADepartment of Earth and Planetary Science, University of California at Berkeley, Berkeley, CA, USAMethyl peroxy nitrate (CH<sub>3</sub>O<sub>2</sub>NO<sub>2</sub>) is a non-acyl peroxy nitrate that is important for photochemistry at low temperatures characteristic of the upper troposphere. We report the first measurements of CH<sub>3</sub>O<sub>2</sub>NO<sub>2</sub>, which we achieved through a new aircraft inlet configuration, combined with thermal-dissociation laser-induced fluorescence (TD-LIF) detection of NO<sub>2</sub>, and describe the accuracy, specificity, and interferences to CH<sub>3</sub>O<sub>2</sub>NO<sub>2</sub> measurements. CH<sub>3</sub>O<sub>2</sub>NO<sub>2</sub> is predicted to be a ubiquitous interference to upper-tropospheric NO<sub>2</sub> measurements. We describe an experimental strategy for obtaining NO<sub>2</sub> observations free of the CH<sub>3</sub>O<sub>2</sub>NO<sub>2</sub> interference. Using these new methods, we made observations during two recent aircraft campaigns: the Deep Convective Clouds and Chemistry (DC-3) and the Studies of Emissions and Atmospheric Composition, Clouds, and Climate Coupling by Regional Surveys (SEAC4RS) experiments. The CH<sub>3</sub>O<sub>2</sub>NO<sub>2</sub> measurements we report have a detection limit (<i>S/N</i> = 2) of 15 pptv at 1 min averaging on a background of 200 pptv NO<sub>2</sub> and an accuracy of ±40%. Observations are used to constrain the interference of pernitric acid (HO<sub>2</sub>NO<sub>2</sub>) to the CH<sub>3</sub>O<sub>2</sub>NO<sub>2</sub> measurements, as HO<sub>2</sub>NO<sub>2</sub> partially decomposes (~11%) along with CH<sub>3</sub>O<sub>2</sub>NO<sub>2</sub> in the heated CH<sub>3</sub>O<sub>2</sub>NO<sub>2</sub> channel used to detect CH<sub>3</sub>O<sub>2</sub>NO<sub>2</sub>.http://www.atmos-meas-tech.net/8/987/2015/amt-8-987-2015.pdf
collection DOAJ
language English
format Article
sources DOAJ
author B. A. Nault
C. Garland
S. E. Pusede
P. J. Wooldridge
K. Ullmann
S. R. Hall
R. C. Cohen
spellingShingle B. A. Nault
C. Garland
S. E. Pusede
P. J. Wooldridge
K. Ullmann
S. R. Hall
R. C. Cohen
Measurements of CH<sub>3</sub>O<sub>2</sub>NO<sub>2</sub> in the upper troposphere
Atmospheric Measurement Techniques
author_facet B. A. Nault
C. Garland
S. E. Pusede
P. J. Wooldridge
K. Ullmann
S. R. Hall
R. C. Cohen
author_sort B. A. Nault
title Measurements of CH<sub>3</sub>O<sub>2</sub>NO<sub>2</sub> in the upper troposphere
title_short Measurements of CH<sub>3</sub>O<sub>2</sub>NO<sub>2</sub> in the upper troposphere
title_full Measurements of CH<sub>3</sub>O<sub>2</sub>NO<sub>2</sub> in the upper troposphere
title_fullStr Measurements of CH<sub>3</sub>O<sub>2</sub>NO<sub>2</sub> in the upper troposphere
title_full_unstemmed Measurements of CH<sub>3</sub>O<sub>2</sub>NO<sub>2</sub> in the upper troposphere
title_sort measurements of ch<sub>3</sub>o<sub>2</sub>no<sub>2</sub> in the upper troposphere
publisher Copernicus Publications
series Atmospheric Measurement Techniques
issn 1867-1381
1867-8548
publishDate 2015-02-01
description Methyl peroxy nitrate (CH<sub>3</sub>O<sub>2</sub>NO<sub>2</sub>) is a non-acyl peroxy nitrate that is important for photochemistry at low temperatures characteristic of the upper troposphere. We report the first measurements of CH<sub>3</sub>O<sub>2</sub>NO<sub>2</sub>, which we achieved through a new aircraft inlet configuration, combined with thermal-dissociation laser-induced fluorescence (TD-LIF) detection of NO<sub>2</sub>, and describe the accuracy, specificity, and interferences to CH<sub>3</sub>O<sub>2</sub>NO<sub>2</sub> measurements. CH<sub>3</sub>O<sub>2</sub>NO<sub>2</sub> is predicted to be a ubiquitous interference to upper-tropospheric NO<sub>2</sub> measurements. We describe an experimental strategy for obtaining NO<sub>2</sub> observations free of the CH<sub>3</sub>O<sub>2</sub>NO<sub>2</sub> interference. Using these new methods, we made observations during two recent aircraft campaigns: the Deep Convective Clouds and Chemistry (DC-3) and the Studies of Emissions and Atmospheric Composition, Clouds, and Climate Coupling by Regional Surveys (SEAC4RS) experiments. The CH<sub>3</sub>O<sub>2</sub>NO<sub>2</sub> measurements we report have a detection limit (<i>S/N</i> = 2) of 15 pptv at 1 min averaging on a background of 200 pptv NO<sub>2</sub> and an accuracy of ±40%. Observations are used to constrain the interference of pernitric acid (HO<sub>2</sub>NO<sub>2</sub>) to the CH<sub>3</sub>O<sub>2</sub>NO<sub>2</sub> measurements, as HO<sub>2</sub>NO<sub>2</sub> partially decomposes (~11%) along with CH<sub>3</sub>O<sub>2</sub>NO<sub>2</sub> in the heated CH<sub>3</sub>O<sub>2</sub>NO<sub>2</sub> channel used to detect CH<sub>3</sub>O<sub>2</sub>NO<sub>2</sub>.
url http://www.atmos-meas-tech.net/8/987/2015/amt-8-987-2015.pdf
work_keys_str_mv AT banault measurementsofchsub3subosub2subnosub2subintheuppertroposphere
AT cgarland measurementsofchsub3subosub2subnosub2subintheuppertroposphere
AT sepusede measurementsofchsub3subosub2subnosub2subintheuppertroposphere
AT pjwooldridge measurementsofchsub3subosub2subnosub2subintheuppertroposphere
AT kullmann measurementsofchsub3subosub2subnosub2subintheuppertroposphere
AT srhall measurementsofchsub3subosub2subnosub2subintheuppertroposphere
AT rccohen measurementsofchsub3subosub2subnosub2subintheuppertroposphere
_version_ 1725350789716639744