O. Reitebuch et al., Nocturnal secondary ozone concentration maxima analysed by sodar observations and surface measurements, ATMOS ENVIR, 34(25), 2000, pp. 4315-4329
The occurrence of nocturnal secondary ozone maxima was investigated by grou
nd-level meteorological and air quality measurements in an urban park in Es
sen, Germany, during 29 individual summer measurement campaigns between May
1995 and September 1997. In addition, during an intensive measurement camp
aign in May 1997, SODAR measurements of wind and turbulence were made. The
spatial and temporal distribution of nocturnal ozone maxima within the meas
urement network of the Environmental Protection Office of North Rhine-Westp
halia was also analysed. Two case studies of nocturnal secondary ozone maxi
ma are discussed in more detail. They represent two different types of this
phenomenon, associated with a nocturnal low-level jet (LLJ) and the passag
e of a front, respectively. In both cases, the nocturnal increase in ozone
concentration was accompanied by a significant increase in the standard dev
iation of the vertical wind speed sigma(w) across the lower stable boundary
layer, indicating enhanced vertical mixing. During the LLJ case, ozone max
ima were observed at 33% of the stations of the Environmental Protection Of
fice network at approximately the same time. In the case of the front, the
time of the ozone concentration rise could be allocated to the time of the:
passage of the front, moving from northwest to southeast across the study
area. For the first time, the measurements presented here document turbulen
t mixing induced by shear forces in the whole layer between the core of the
LLJ and the ground surface during secondary nocturnal ozone maxima. (C) 20
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