Open AccessMeasurement of atmospheric NO 2 by pulsed cavity ring‐down spectroscopy
Author(s) -
Osthoff Hans D.,
Brown Steven S.,
Ryerson Thomas B.,
Fortin Tara J.,
Lerner Brian M.,
Williams Eric J.,
Pettersson Anders,
Baynard Tahllee,
Dubé William P.,
Ciciora Steven J.,
Ravishankara A. R.
Publication year - 2006
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/2005jd006942
Subject(s) - cavity ring down spectroscopy , nitrogen dioxide , analytical chemistry (journal) , calibration , detection limit , ozone , absorption (acoustics) , environmental science , atmosphere (unit) , spectrometer , parts per notation , absorption spectroscopy , materials science , optics , meteorology , chemistry , physics , environmental chemistry , organic chemistry , chromatography , quantum mechanics
We have constructed a pulsed cavity ring‐down spectrometer (CARDS) for simultaneous measurements of nitrogen dioxide (NO 2 ), the nitrate radical (NO 3 ), and dinitrogen pentoxide (N 2 O 5 ) in the atmosphere. In this paper, we describe the development of the instrument to measure NO 2 via its absorption at 532 nm. The NO 2 detection channel was calibrated against a NIST traceable calibration standard as well as a photolysis‐chemiluminescence (P‐CL) NO 2 detector. The absorption cross section of NO 2 at 532 nm was determined to be (1.45 ± 0.06) × 10 −19 cm 2 . The NO 2 detection limit (1σ) for 1 s data is 40 pptv, and the instrument response is accurate within ±4% (1σ) under laboratory conditions. The linear dynamic range of the instrument has been verified from the detection limit to above 200 ppbv (r 2 > 99.99%). For field measurements it is necessary to correct the CARDS NO 2 signal for absorption by ozone. Under ambient conditions we report 1 s NO 2 CARDS data with total uncertainty ±(4%, 60 pptv + 0.4 × (pptv/ppbv) × O 3 ) (1σ). The instrument was deployed in the field during the New England Air Quality Study–International Transport and Chemical Transformation on board the NOAA research vessel Ronald H. Brown in the summer of 2004 and in Boulder, Colorado, in the winter of 2005. In both campaigns, CARDS and P‐CL NO 2 measurements were highly correlated (r 2 > 98%), indicating the absence of interfering gas phase absorbers at 532 nm other than ozone and the suitability of CARDS to measure NO 2 in the troposphere.