A relaxed eddy accumulation system for measuring vertical fluxes of nitrous acid

A relaxed eddy accumulation (REA) system combined with a nitrous acid (HONO) analyzer was developed to measure atmospheric HONO vertical fluxes. The system consists of three major components: (1) a fast-response sonic anemometer measuring both vertical wind velocity and air temperature, (2) a fast-r...

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Main Authors: X. Ren, J. E. Sanders, A. Rajendran, R. J. Weber, A. H. Goldstein, S. E. Pusede, E. C. Browne, K.-E. Min, R. C. Cohen
Format: Article
Language:English
Published: Copernicus Publications 2011-10-01
Series:Atmospheric Measurement Techniques
Online Access:http://www.atmos-meas-tech.net/4/2093/2011/amt-4-2093-2011.pdf
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author X. Ren
J. E. Sanders
A. Rajendran
R. J. Weber
A. H. Goldstein
S. E. Pusede
E. C. Browne
K.-E. Min
R. C. Cohen
author_facet X. Ren
J. E. Sanders
A. Rajendran
R. J. Weber
A. H. Goldstein
S. E. Pusede
E. C. Browne
K.-E. Min
R. C. Cohen
author_sort X. Ren
collection DOAJ
description A relaxed eddy accumulation (REA) system combined with a nitrous acid (HONO) analyzer was developed to measure atmospheric HONO vertical fluxes. The system consists of three major components: (1) a fast-response sonic anemometer measuring both vertical wind velocity and air temperature, (2) a fast-response controlling unit separating air motions into updraft and downdraft samplers by the sign of vertical wind velocity, and (3) a highly sensitive HONO analyzer based on aqueous long path absorption photometry that measures HONO concentrations in the updrafts and downdrafts. A dynamic velocity threshold (±0.5σ<sub>w</sub>, where σ<sub>w</sub> is a standard deviation of the vertical wind velocity) was used for valve switching determined by the running means and standard deviations of the vertical wind velocity. Using measured temperature as a tracer and the average values from two field deployments, the flux proportionality coefficient, <i>β</i>, was determined to be 0.42 ± 0.02, in good agreement with the theoretical estimation. The REA system was deployed in two ground-based field studies. In the California Research at the Nexus of Air Quality and Climate Change (CalNex) study in Bakersfield, California in summer 2010, measured HONO fluxes appeared to be upward during the day and were close to zero at night. The upward HONO flux was highly correlated to the product of NO<sub>2</sub> and solar radiation. During the Biosphere Effects on Aerosols and Photochemistry Experiment (BEARPEX 2009) at Blodgett Forest, California in July 2009, the overall HONO fluxes were small in magnitude and were close to zero. Causes for the different HONO fluxes in the two different environments are briefly discussed.
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spelling doaj.art-213bf70ea5af4b6f9bb8630ce201cfb62022-12-21T20:37:16ZengCopernicus PublicationsAtmospheric Measurement Techniques1867-13811867-85482011-10-014102093210310.5194/amt-4-2093-2011A relaxed eddy accumulation system for measuring vertical fluxes of nitrous acidX. RenJ. E. SandersA. RajendranR. J. WeberA. H. GoldsteinS. E. PusedeE. C. BrowneK.-E. MinR. C. CohenA relaxed eddy accumulation (REA) system combined with a nitrous acid (HONO) analyzer was developed to measure atmospheric HONO vertical fluxes. The system consists of three major components: (1) a fast-response sonic anemometer measuring both vertical wind velocity and air temperature, (2) a fast-response controlling unit separating air motions into updraft and downdraft samplers by the sign of vertical wind velocity, and (3) a highly sensitive HONO analyzer based on aqueous long path absorption photometry that measures HONO concentrations in the updrafts and downdrafts. A dynamic velocity threshold (±0.5σ<sub>w</sub>, where σ<sub>w</sub> is a standard deviation of the vertical wind velocity) was used for valve switching determined by the running means and standard deviations of the vertical wind velocity. Using measured temperature as a tracer and the average values from two field deployments, the flux proportionality coefficient, <i>β</i>, was determined to be 0.42 ± 0.02, in good agreement with the theoretical estimation. The REA system was deployed in two ground-based field studies. In the California Research at the Nexus of Air Quality and Climate Change (CalNex) study in Bakersfield, California in summer 2010, measured HONO fluxes appeared to be upward during the day and were close to zero at night. The upward HONO flux was highly correlated to the product of NO<sub>2</sub> and solar radiation. During the Biosphere Effects on Aerosols and Photochemistry Experiment (BEARPEX 2009) at Blodgett Forest, California in July 2009, the overall HONO fluxes were small in magnitude and were close to zero. Causes for the different HONO fluxes in the two different environments are briefly discussed.http://www.atmos-meas-tech.net/4/2093/2011/amt-4-2093-2011.pdf
spellingShingle X. Ren
J. E. Sanders
A. Rajendran
R. J. Weber
A. H. Goldstein
S. E. Pusede
E. C. Browne
K.-E. Min
R. C. Cohen
A relaxed eddy accumulation system for measuring vertical fluxes of nitrous acid
Atmospheric Measurement Techniques
title A relaxed eddy accumulation system for measuring vertical fluxes of nitrous acid
title_full A relaxed eddy accumulation system for measuring vertical fluxes of nitrous acid
title_fullStr A relaxed eddy accumulation system for measuring vertical fluxes of nitrous acid
title_full_unstemmed A relaxed eddy accumulation system for measuring vertical fluxes of nitrous acid
title_short A relaxed eddy accumulation system for measuring vertical fluxes of nitrous acid
title_sort relaxed eddy accumulation system for measuring vertical fluxes of nitrous acid
url http://www.atmos-meas-tech.net/4/2093/2011/amt-4-2093-2011.pdf
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