1987
DOI: 10.1007/bf00048859
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Measurements of tropospheric OH concentrations: A comparison of field data with model predictions

Abstract: Abstract. Using long path UV absorption spectroscopy we have measured OH concentrations close to the earth's surface. The OH values observed at two locations in Germany during 1980 through 1983 range from 0.7 x 1()6 to 3.2 x 10" cm-3 • Simultaneously we measured the concentrations of 03, H20, NO, N02, CH 4 , CO, and the light non methane hydrocarbons. We also determined the photolysis rates of 0 3 and N0 2 • This allows calculations of OH using a zero dimensional time dependent model. The modelled OH concentra… Show more

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Cited by 118 publications
(52 citation statements)
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“…The ambient measurement of OH is therefore a good test of proposed chemical mechanisms postulating the importance of chemical species and/or processes in the atmosphere. The OH radical is usually measured in the field with one of three techniques: differential optical absorption spectroscopy (DOAS; Perner et al, 1987) via absorption of light by OH, chemical ionisation mass spectrometry (CIMS; Eisele and Tanner, 1991) via the detection of H 2 SO 4 after the oxidation of SO 2 by atmospheric OH, and laser-induced fluorescence (LIF-FAGE;Hard et al, 1984) via the detection of OH radical fluorescence after laser excitation. Several comparison campaigns have been performed, both on ground (Hofzumahaus et al, 1998;Schlosser et al, 2007) and aircraft (Eisele et al, 2001;Ren et al, 2012), to test the consistency and performance of the different techniques and have generally shown good agreement.…”
Section: Introductionmentioning
confidence: 99%
“…The ambient measurement of OH is therefore a good test of proposed chemical mechanisms postulating the importance of chemical species and/or processes in the atmosphere. The OH radical is usually measured in the field with one of three techniques: differential optical absorption spectroscopy (DOAS; Perner et al, 1987) via absorption of light by OH, chemical ionisation mass spectrometry (CIMS; Eisele and Tanner, 1991) via the detection of H 2 SO 4 after the oxidation of SO 2 by atmospheric OH, and laser-induced fluorescence (LIF-FAGE;Hard et al, 1984) via the detection of OH radical fluorescence after laser excitation. Several comparison campaigns have been performed, both on ground (Hofzumahaus et al, 1998;Schlosser et al, 2007) and aircraft (Eisele et al, 2001;Ren et al, 2012), to test the consistency and performance of the different techniques and have generally shown good agreement.…”
Section: Introductionmentioning
confidence: 99%
“…Since the first successful measurement of tropospheric OH radicals by long-path laser absorption in the early 1980s (Perner et al, 1987) several instruments based on different detection principles were developed (for an overview see Crosley, 1994). Among those only the spectroscopic detection of OH by long-path laser absorption provides absolutely calibrated OH measurements.…”
Section: Introductionmentioning
confidence: 99%
“…Initial attempts to measure atmospheric OH by DOAS were successful, but required very long absorption path lengths (10 km) and long integration times of about 1 h (Perner et al, 1987;Platt et al, 1988). Attempts in the 1970s and 1980s to measure atmospheric OH by LIF and the radiocarbon tracer method failed as a result of insufficient detection sensitivity, poor technical performance or interference problems.…”
Section: Introductionmentioning
confidence: 99%