Open AccessGround‐based comparison of NO 2 , H 2 O, and O 3 measured by long‐path and in situ techniques during the 1993 Tropospheric OH Photochemistry Experiment
Author(s) -
Harder J. W.,
Williams E. J.,
Baumann K.,
Fehsenfeld F. C.
Publication year - 1997
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 - 10.1029/96jd01729
Subject(s) - differential optical absorption spectroscopy , troposphere , trace gas , mixing ratio , ozone , environmental science , observatory , atmospheric sciences , retroreflector , atmospheric chemistry , analytical chemistry (journal) , absorption (acoustics) , meteorology , geology , chemistry , environmental chemistry , physics , optics , laser , astrophysics
One of the major objectives of the 1993 Tropospheric OH Photochemistry Experiment (August 8 to October 4, 1993) was to compare atmospheric measurements of the important trace gas species NO 2 , O 3 , and H 2 O by in situ techniques and by long‐path differential absorption spectroscopy. These compounds were measured over a 20.6 km folded optical path from Fritz Peak Observatory to Caribou Mine where a retroreflector array is located. In situ measurements were made at Idaho Hill, 0.7 km northwest of Caribou Mine and 25 km west of Boulder, Colorado. NO 2 was determined at Idaho Hill by photolysis followed by NO chemiluminescence. O 3 and H 2 O were measured at this site using calibrated commercial instruments. Using fractional differences ([long path ‐ Idaho Hull]/Idaho Hill) as a measure of agreement, overall agreement for ozone and water are +3±7% and −4±17%, respectively. For NO 2 the comparison is complicated by the influence of strong sources and large ambient variability during the measurements. During times of clean westerly flow, fractional differences of +30±110% were observed. Further analysis of the data to evaluate these biases show that for mixing ratios greater than 300 pptv (well above the 1σ detection limit of 30–45 pptv) the two methods differ by no more than 10%, a value well within the combined uncertainties of the measurement techniques.