By Young J. Kim, Ulrich Platt
This e-book offers with fresh advancements and functions of environmental tracking applied sciences, with emphasis on quickly progressing optical and organic equipment. Written through all over the world specialists, this ebook could be of curiosity to environmental scientists in academia, study institutes, and the govt..
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Some of the oxidation products lead to the formation of organic peroxy- and HO2 radicals, which in turn can yield OH radicals. Since the formation of NO3 does not require sunlight, this OH source will also be active at night time. Among the first indications for the involvement of chlorine species in the formation of the Antarctic ozone hole was the detection of OClO by ZSLDOAS (Solomon et al. 1987). Also BrO could since be detected in stratospheric air (Solomon et al. 1989; Wahner et al. 1990; Richter et al.
92, 8329–8338. L. (1989), Visible and nearultraviolet spectroscopy at McMurdo station, Antarctica: 5. Observations of the diurnal variations of BrO and OClO, J. Geophys. , 94, 11393–11403. L. (1998), Broadband lidar measurements of tropospheric water vapour profiles, J. Geophys. , 103, 31191–31202. Stutz J. and Platt U. (1996), Numerical analysis and error estimation of differential optical absorption spectroscopy measurements with least squares methods, Appl. Optics, 35, 6041–6053. , and Barrie L.
Advanced Environmental Monitoring by Young J. Kim, Ulrich Platt