Picture of two heads

Open Access research that challenges the mind...

The Strathprints institutional repository is a digital archive of University of Strathclyde research outputs. Strathprints provides access to thousands of Open Access research papers by University of Strathclyde researchers, including those from the School of Psychological Sciences & Health - but also papers by researchers based within the Faculties of Science, Engineering, Humanities & Social Sciences, and from the Strathclyde Business School.

Discover more...

Effect of long-range transport on local PM10 concentrations in the UK

Beverland, I J and Tunes, T and Sozanska, M and Elton, R. and Agius, R and Heal, M R (2000) Effect of long-range transport on local PM10 concentrations in the UK. International Journal of Environmental Health Research, 10 (3). pp. 229-238. ISSN 0960-3123

Full text not available in this repository. (Request a copy from the Strathclyde author)


This study describes the effects of long-range transport of secondary airborne particles on local PM10 levels in Edinburgh (UK) during the period 1 January to 31 March 1996. Air mass back trajectories for each day were grouped into six atmospheric transport patterns to examine their influences on local PM10 concentrations. Significant differences in receptor PM10 concentrations were observed between the trajectory patterns (p = 0.1%). Air masses from Eastern Europe resulted in higher daily PM10 averages than any of the other patterns (p = 1.0%). Median PM10 concentrations in Edinburgh increased by 10-15 mu g m(-3) when air mass trajectories were from these regions. This effect should be considered by local authorities to acknowledge that not all PM10 sources are possible to control in local air quality management areas. Further evidence of the influence of long-range transport was found by detailed examination of the concurrent development of a pollution episode in Edinburgh, London and Belfast. Differences in the temporal development of the episode in the three cities were attributed to trajectory variations in the proximity of frontal weather systems.