Long-Term Trends of Lead-210 Concentrations in the Ground-Level Air in Finland and Bulgaria

Author(s):  
Jussi Paatero ◽  
Blagorodka Veleva ◽  
Juha Hatakka
Radiocarbon ◽  
1995 ◽  
Vol 37 (3) ◽  
pp. 961-962 ◽  
Author(s):  
Sylvius Hartwig

In a recent paper (Hartwig, ms.) I have shown that it is possible to understand and discuss the changing Austausch (i.e., exchange of air parcels between different atmospheric layers) between the stratosphere and troposphere by means of long-term measurement of series of spallation products. It is well known (Friend 1961; Müh et al. 1966; Hartwig et al. 1969) that there is a seasonal pattern in the 7Be concentration of ground-level air with a maximum during May–June. This maximum is caused by enhanced exchange processes between the atmospheric compartments of the stratosphere and troposphere during this interval. Generally, those exchange processes are a consequence of stability and dynamics of the atmospheric compartments, which themselves result from, among other factors, the distribution of the heat sources in those compartments, namely the ground and the ozone layer.


2018 ◽  
Vol 10 (9) ◽  
pp. 3330 ◽  
Author(s):  
Iván Hernández-Paniagua ◽  
Rodrigo Lopez-Farias ◽  
José Piña-Mondragón ◽  
Juan Pichardo-Corpus ◽  
Olivia Delgadillo-Ruiz ◽  
...  

Here, we present an assessment of long-term trends in the O3 weekend effect (WE) occurrences and spread within the Mexico City (MCMA), Guadalajara (GMA), and Monterrey (MMA) metropolitan areas, which are the three largest metropolitan areas (MAs) of Mexico and concentrate around 33% of the total population in the country. Daytime averages and peak differences in O3 concentrations from weekdays to weekends were used as a proxy of WE occurrence. All MAs exhibited the occurrence of WE in all years at least in one monitoring site. Substantial differences in O3 daytime averages and peaks from weekdays to weekends have decreased over time in all MAs, and since 1998 and 2013 for the MCMA and GMA, respectively, higher O3 levels during weekends are typical during most of the year. The largest variations in the O3 WE were observed at downwind and urban core sites of the MCMA and GMA. Significant increasing trends (p < 0.05) in the O3 WE magnitude were observed for Sundays at all sites within the MCMA, with trends in annual averages ranging between 0.33 and 1.29 ppb O3 yr−1. Within the GMA, for Sundays, fewer sites exhibited increasing trends in the WE occurrence and at lower growth rates (0.32 and 0.48 ppb yr−1, p < 0.1) than within the MCMA, while within the MMA no apparent trends were observed in marked contrast with the MCMA and GMA. Our findings suggest that policies implemented have been successful in controlling weekday ground-level O3 within the MCMA and GMA, but further actions must be introduced to control the increases in the O3 WE magnitude and spread.


Nature ◽  
1966 ◽  
Vol 210 (5036) ◽  
pp. 579-580 ◽  
Author(s):  
B. SHLEIEN ◽  
A. G. FRIEND

2017 ◽  
Vol 2 (2) ◽  
Author(s):  
Jussi Paatero ◽  
Blagorodka Veleva ◽  
Elena Hristova ◽  
Juha Hatakka

1998 ◽  
Vol 103 (D1) ◽  
pp. 1471-1480 ◽  
Author(s):  
Arlene M. Fiore ◽  
Daniel J. Jacob ◽  
Jennifer A. Logan ◽  
Jeffrey H. Yin

2014 ◽  
Vol 68 (1) ◽  
pp. 83-88 ◽  
Author(s):  
Marija Jankovic ◽  
Dragana Todorovic ◽  
Jelena Nikolic ◽  
Milica Rajacic ◽  
Gordana Pantelic ◽  
...  

7Be, 210Pb and 137Cs activity concentrations in ground level air at five monitoring stations (MS Vinca, Zeleno Brdo, Zajecar, Vranje and Zlatibor) in Serbia were determined during the period from May 2011. to September 2012., as part of the project monitoring of Serbia. Activity of the radionuclides in air was determined on an HPGe detector (Canberra, relative efficiency 20 %) by standard gamma spectrometry. Concentrations of cosmogenic 7Be, ranged from 1.5 to 8.8 mBq m-3 and exhibit maxima in the spring/summer period. The maximum concentrations for 210Pb were generally obtained in the fall for all investigated locations, and concentrations were in range 3.6 - 30 ? 10-4 Bq m-3. The activity concentrations of anthropogenic 137Cs in ground level air, during the observed period, were at level 0.3 - 8 ?Bq m-3. The variations in 7Be/210Pb activity ratio for the investigated stations are also presented.


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