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  • 1
    In: Journal of Geophysical Research: Atmospheres, American Geophysical Union (AGU), Vol. 105, No. D1 ( 2000-01-20), p. 1563-1583
    Abstract: The Schauinsland Ozone Precursor Experiment (SLOPE96) campaign was conducted in June 1996 to study the physicochemical transformation of pollutants and the production of photooxidants during transport from the city of Freiburg to the Schauinsland mountain. For this purpose, chemical surface measurements were made at the entrance of the valley Großes Tal, and close to the Schauinsland summit, at 1200 m altitude on a saddle at the end of the valley. In addition, measurements of ozone, NO 2 , and meteorological parameters were made on two tethered balloons and aboard a small aircraft. This paper describes the experimental setup and the measurements of ozone, odd‐nitrogen compounds, carbonyl compounds, CO, and photolysis frequencies made during SLOPE96. The various instruments used on the different platforms were harmonized on the basis of intercomparison experiments in order to achieve a consistent picture. Large precursor concentrations from the nearby city of Freiburg are transported to Schauinsland in a valley wind system during stagnant high‐pressure conditions. These conditions occurred only on 2 days of the campaign, and only 1 day (June 5) was predictable enough to allow for deployment of the aircraft and the balloons. An OH concentration of 8 ‐ 10× 0 6 cm −3 is derived from the rate of change of HNO 3 and NO 2 on June 5 at Schauinsland (1.5–3 ppb NO 2 ; J O1 D ≈ 2 × 10 −5 s −1 ), assuming quasi steady state and a homogeneous air mass. The ozone production rate as determined from the photostationary state of NO x at Schauinsland reached maximum daily values between 15 and 60 ppb h 1 around noontime. On average, P(O 3 ) comprised about 30% of the photolysis rate of NO 2 . Similar to earlier observations at Schauinsland, a good correlation between P(O 3 ) and the product of UV radiation and precursor concentrations was found.
    Type of Medium: Online Resource
    ISSN: 0148-0227
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 2000
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    detail.hit.zdb_id: 3094181-7
    detail.hit.zdb_id: 3094219-6
    detail.hit.zdb_id: 3094167-2
    detail.hit.zdb_id: 2220777-6
    detail.hit.zdb_id: 3094197-0
    SSG: 16,13
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  • 2
    Online Resource
    Online Resource
    Elsevier BV ; 2009
    In:  International Journal of Hygiene and Environmental Health Vol. 212, No. 2 ( 2009-3), p. 146-156
    In: International Journal of Hygiene and Environmental Health, Elsevier BV, Vol. 212, No. 2 ( 2009-3), p. 146-156
    Type of Medium: Online Resource
    ISSN: 1438-4639
    Language: English
    Publisher: Elsevier BV
    Publication Date: 2009
    detail.hit.zdb_id: 2039765-3
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  • 3
    Online Resource
    Online Resource
    Elsevier BV ; 2002
    In:  Journal of Chromatography A Vol. 963, No. 1-2 ( 2002-7), p. 225-230
    In: Journal of Chromatography A, Elsevier BV, Vol. 963, No. 1-2 ( 2002-7), p. 225-230
    Type of Medium: Online Resource
    ISSN: 0021-9673
    RVK:
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    RVK:
    Language: English
    Publisher: Elsevier BV
    Publication Date: 2002
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    detail.hit.zdb_id: 1171488-8
    SSG: 11
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  • 4
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 2000
    In:  Journal of Geophysical Research: Atmospheres Vol. 105, No. D1 ( 2000-01-20), p. 1611-1622
    In: Journal of Geophysical Research: Atmospheres, American Geophysical Union (AGU), Vol. 105, No. D1 ( 2000-01-20), p. 1611-1622
    Abstract: The concentration of hydroxyl radicals is estimated from the degradation of NO x and selected volatile organic compounds (VOCs) during the transport of polluted air masses from the city of Freiburg to the Schauinsland mountain through a steep valley called “Großes Tal.” The approach is based upon chemical and meteorological measurements made during the Schauinsland Ozone Precursor Experiment (SLOPE96) at two ground‐based sites and aboard a small aircraft. Separation of chemistry and transport is achieved through the degradation of chemical compounds with significantly different reactivity towards OH. The transport time of the air between the two measurements (90±5 min) and the influence of mixing with background air on the calculated OH concentration is quantified with the help of a dispersion experiment with SF 6 and from airborne chemical measurements. The OH concentration (7– 0 × 10 6 cm −3 ) is almost a factor of 2 larger than what is calculated with a chemical box model constrained by the measured trace gas concentrations and photolysis rates. The radical budget can be closed within the experimental uncertainties, when an upper limit is adopted for the photolysis of nitrous acid, in addition to the radical production from photolysis of ozone, H 2 O 2 , and carbonyl compounds as well as ozonolysis of unsaturated VOCs. Biogenic VOCs (i.e., isoprene, terpenes, and a number of oxidated compounds) comprise about half of the total VOC reactivity in the transported plume. The results from SLOPE96 confirm the assumptions made in the analysis of an earlier experiment conducted in 1992, when noontime OH concentrations of 6 ‐ 8×10 6 cm −3 were derived in the presence of NO x mixing ratios between 70 ppb at the entrance of the valley and 15 ppb at Schauinsland. Comparison with direct measurements from different studies qualitatively reveals the expected dependence of [OH] on the NO 2 mixing ratio with a maximum around 1–2 ppb of NO 2 .
    Type of Medium: Online Resource
    ISSN: 0148-0227
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 2000
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    SSG: 16,13
    Library Location Call Number Volume/Issue/Year Availability
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