Department of Climatology and Atmosphere Protection, Wrocław University, ul. Kosiby 6/8, 51-621 Wrocław, Poland.
J Environ Manage. 2012 Oct 30;109:70-9. doi: 10.1016/j.jenvman.2012.04.048. Epub 2012 Jun 9.
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 2000-2009 for nitrogen compounds. In the UK, emission abatements influence the national deposition budget to a larger extent than meteorological changes (except for NH(x)). 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.
大气环流和降雨是控制大气污染物沉积的重要因素。本文旨在通过英国和波兰的案例研究,定量分析这些因素在硫和氮化合物沉积中的作用。使用 FRAME 模型计算了基础年(2005 年)、干燥年(英国为 2003 年,波兰为 1974 年)和湿润年(英国为 2000 年,波兰为 2003 年)以及年风型对比年(英国为 1986 年和 1996 年,波兰为 1998 年和 1996 年)的沉积量。年风型和降雨的变化导致两国硫和氮化合物沉积的空间格局和国家沉积量预算发生了具有统计学意义的变化。在这两个国家,如果考虑到干燥年,S 和 N 的沉积预算分别比参考年低 5%。对于湿润年,全国总沉积量增加最多可达 17%。与东部风频率增加相关的国家沉积量增加可达 14%(波兰)和 8%(英国)。国家沉积预算低于高西风频率年份的平均值,尤其是英国(高达 13%)。湿沉积受气象因素的影响比干沉积大。在波兰,由于气象因素导致的国家沉积预算变化大于 2000-2009 年氮化合物减排引起的变化。在英国,排放减少对国家沉积预算的影响大于气象变化(除 NH(x) 外)。这些发现与未来气候变化有关,特别是考虑到年降水量的潜在增加。这可能导致在高山地区,特别是在有大量硫和氮负荷的山区,沉积量增加。年风速和频率的变化可以改变沉积的空间格局。西风频率的增加将使两国受益,减少 S 和 N 的沉积。波兰和英国的 NW 地区在东风增强的年份,沉积量将高于平均水平,这可能导致目前受酸化和富营养化保护的地区,酸和氮沉积的临界负荷超过极限,尽管正在进行减排。