Kryza, Maciej; Werner, Malgorzata; Dore, Anthony J.; Blas, Marek; Sobik, Mieczyslaw. 2012 The role of annual circulation and precipitation on national scale deposition of atmospheric sulphur and nitrogen compounds. Journal of Environmental Management, 109. 70-79. 10.1016/j.jenvman.2012.04.048
Abstract
Atmospheric circulation and rainfall are important factors controlling the deposition of atmospheric
pollutants. This paper aims to quantify the role of these factors in the deposition of sulphur and nitrogen
compounds, using case studies in the United Kingdom and Poland. The FRAME model has been applied to
calculate deposition for the base year (2005), dry and wet years (2003 and 2000 for the UK and 2003 and
1974 for Poland, respectively), and for years with contrasting annual wind patterns (1986 and 1996 for
the UK, and 1998 and 1996 for Poland).
Variation in annual wind and rainfall resulted in statistically significant changes in spatial patterns of
deposition and the national deposition budget of sulphur and nitrogen compounds in both countries. The
deposition budgets of S and N are 5% lower than for the reference year if the dry year is considered in
both countries. For the wet year, there is an increase in country total deposition by up to 17%. Years with
an increased frequency of eastern winds are associated with an increase in deposition of up to 14% in
Poland and 8% in the UK. The national deposition budget is below the average for the years with high
frequencies of W winds, especially for the UK (up to 13%). Wet deposition varies due to meteorological
factors to a larger extent than dry deposition. In Poland, the changes in national deposition budget due to
meteorological factors exceed the changes resulting from emission abatements in years 2000e2009 for
nitrogen compounds. In the UK, emission abatements influence the national deposition budget to
a larger extent than meteorological changes (except for NHx).
The findings are important in relation to future climate changes, especially considering the potential
increase in annual precipitation. This may lead to an increase in deposition over mountainous areas with
sensitive ecosystems, where annual rainfall brings significant load of S and N. Changes in annual wind
speed and frequency can modify the spatial pattern of deposition. An increased frequency of W winds
will benefit both countries through reduced S and N deposition. NW areas of Poland and the UK will
suffer from above-average deposition during years with enhanced easterly flow, and this may result in
critical loads for acid and nitrogen deposition being exceeded over the areas that are at present sufficiently
protected from acidification and eutrophication, despite the ongoing emission abatements.
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