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With respect to the atmospheric budget of molecular hydrogen (H₂), Kraków represents a typical central European urban agglomeration with intense traffic and a relatively high proportion of low-level emissions associated with burning of fossil fuel (mainly coal and gas) for heating. The vehicle fleet in the city still contains a relatively high fraction of cars without properly operating catalysts, which constitutes a considerable source of atmospheric hydrogen. The mixing ratios of hydrogen in near-ground atmosphere were measured quasi-continuously over two years (from 01.2007 till 12.2008) at two different locations within the urban area of Kraków: close to the city center and at the outskirts of the city. Although both measurement locations were under the influence of local traffic, they differ with respect to the structure of local terrain (proportions of buildings, roads, and area covered by vegetation), as well as by local micrometeorological conditions. A very wide range of H₂ mixing ratios was observed at both sites, with peak mixing ratios reaching 2,800 ppb. Distinct seasonality of H₂ mixing ratios was observed, with higher values recorded during winter months. Also, distinct daily variations of H₂ levels often were observed, with morning and evening H₂ maxima associated with traffic rush hours. Diurnal variation of hydrogen concentrations at both locations differs seasonally due to different micrometeorological conditions and source patterns, including car traffic intensity.
The high-altitude laboratory of greenhouse gas measurement, KASLAB, was founded on the Polish mountain Kasprowy Wierch in 1994. In the direct neighborhood of the measuring point there are no significant sources of compounds measured at the station. However, the measuring point may be affected by periodic anthropogenic emissions from the nearby Podhale region, with Zakopane the most popular tourist resort (6 km to the north and 1 km below Kasprowy Wierch). Periodic air enrichment in CO content detected at the KASLAB station indicates a prior contact of air masses that reach Kasprowy Wierch with the lower layer of the troposphere and can be used for qualitative and quantitative evaluation of trace gas emissions (for example CO2) from regions with strong anthropopression. Data analysis performed for 2010 presented in this paper revealed that the anthropogenic component of carbon dioxide observed at Kasprowy Wierch usually does not exceed 2 ppm, occasionally reaching a value of 10 ppm. Respiration component of atmospheric CO2 concentration at Kasprowy Wierch can be as high as 35 ppm.
The results of regular observations of atmospheric CO2 mixing ratios, carried out during the period 1996-2006 at two continental sites located in southern Poland, approximately 100 km apart, are presented and discussed. These sites (Kasprowy Wierch, 49°14'N, 19°59'E, 1989 m a.s.l. and Kraków, 50°04'N, 19°55'E, 220 m a.s.l) are located in two contrasting environments: (i) high-altitude mountainous area, relatively free of anthropogenic influences, and (ii) typical urban environment with numerous local sources of carbon dioxide of anthropogenic origin. The mean annual CO2 concentration recorded at Kasprowy Wierch increased from 361.8 ppm in 1997 to 382.7 ppm in 2006. The resulting mean annual growth rate (2.14±0.57 ppm year-1) is slightly higher than that derived for the marine CO2 reference curve (2.02±0.26 ppm year-1), calculated for the latitude band within which Kasprowy Wierch station is located (48.6°N-53.1°N). The CO2 mixing ratios mea­sured in the urban atmosphere revealed quasi-permanent excess concentration of this gas when compared with the regional reference. The mean concentration of CO2 in Kraków for the period 2003-06 was ca. 8.5% high­er than that recorded at the high-altitude mountain site (Kasprowy Wierch).
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