Air Quality Measurement and Analysis Research Section, Atmospheric Science and Technology Directorate, Environment and Climate Change, 4905 Dufferin Street, Toronto, ON, M3H 5T4, Canada.
U.S. Geological Survey, Water Mission Area - Observing Systems Division, Denver Federal Center, Mail Stop 401, Bldg. 95, Box 25046, Denver, CO, 80225, USA.
Environ Monit Assess. 2023 Oct 18;195(11):1333. doi: 10.1007/s10661-023-11771-z.
Wet deposition monitoring is a critical part of the long-term monitoring of acid deposition, which aims to assess the ecological impact of anthropogenic emissions of SO and NO. In North America, long-term wet deposition has been monitored through two national networks: the Canadian Air and Precipitation Monitoring Network (CAPMoN) and the US National Atmospheric Deposition Program (NADP), for Canada and the USA, respectively. In order to assess the comparability of measurements from the two networks, collocated measurements have been made at two sites, one in each country, since 1986 (Sirois et al., in Environmental Monitoring and Assessment, 62, 273-303, 2000; Wetherbee et al., in Environmental Monitoring and Assessment, 1995-2004, 2010). In this study, we compared the measurements from NADP and CAPMoN instrumentation at the collocated sites at the Pennsylvania State University (Penn State), USA, from 1989 to 2016, and Frelighsburg, Quebec, Canada, from 2002 to 2019. We also included in the study the collocated daily-vs-weekly measurements by the CAPMoN network during 1999-2001 and 2016-2017 in order to evaluate the differences in wet concentration of ions due to sampling frequency alone. The study serves as an extension to two previous CAPMoN-NADP inter-comparisons by Sirois et al. (Environmental Monitoring and Assessment, 62, 273-303, 2000) and Wetherbee et al., in (Environmental Monitoring and Assessment, 1995-2004, 2010). At the Penn State University site, for 1986-2019, CAPMoN was higher than NADP for all ions, in terms of weekly concentration, precipitation-weighted annual mean concentration, and annual wet deposition. The precipitation-weighted annual mean concentrations were higher for SO (2%), NO (12%), NH (16%), H (6%), and base cations and Cl (11-15%). For annual wet deposition, CAPMoN was higher for SO, NO, NH and H (5-17%), and base cations and Cl (12-17%) during 1986-2019. At the Frelighsburg site, NADP changed the sample collector in October 2011. For 2002-2011, the relative differences at the Frelighsburg site were positive and similar in magnitude to those at the Penn State site. For 2012-2019, the precipitation-weighted annual mean concentrations were 5-27% lower than NADP, except for H, which was 23% higher. The change in sample collector by NADP had the largest effect on between-network biases. The comparisons of daily-vs-weekly measurements conducted by the CAPMoN network during 1999-2001 and 2016-2017 show that the weekly measurements were higher than the daily measurements by 1-3% for SO, NO, and NH; 3-9% for Ca, Mg, Na, and Cl; 10-24% for K; and lower for H by 8-30% in terms of precipitation-weighted mean concentration. Thus, differences in sampling frequencies did not contribute to the systematically higher CAPMoN measurements. Understanding the biases in the data for these networks is important for interpretation of continental scale deposition models and transboundary comparison of wet deposition trends.
湿沉降监测是酸沉降长期监测的重要组成部分,其目的是评估人为排放的 SO 和 NO 对生态的影响。在北美,通过两个国家网络长期监测湿沉降:加拿大空气和降水监测网络(CAPMoN)和美国国家大气沉降计划(NADP),分别监测加拿大和美国的情况。为了评估这两个网络测量值的可比性,自 1986 年以来,在两国的两个地点(一个在加拿大,一个在美国)进行了同期测量(Sirois 等人,《环境监测与评估》,62,273-303,2000;Wetherbee 等人,《环境监测与评估》,1995-2004,2010)。在本研究中,我们比较了 1989 年至 2016 年美国宾夕法尼亚州立大学(Penn State)和 2002 年至 2019 年加拿大魁北克省弗雷利堡(Frelighsburg)的 NADP 和 CAPMoN 仪器的测量值。我们还将 CAPMoN 网络在 1999-2001 年和 2016-2017 年同期进行的每日与每周测量值包括在研究中,以评估仅由于采样频率不同而导致的离子湿浓度差异。本研究是 Sirois 等人(《环境监测与评估》,62,273-303,2000)和 Wetherbee 等人的两项 CAPMoN-NADP 比较研究的扩展(《环境监测与评估》,1995-2004,2010)。在宾夕法尼亚州立大学,就 1986-2019 年而言,CAPMoN 的每周浓度、降水加权年平均浓度和年湿沉降均高于 NADP。SO(2%)、NO(12%)、NH(16%)、H(6%)和碱金属阳离子和 Cl(11-15%)的降水加权年平均浓度更高。对于年湿沉降,CAPMoN 高于 NADP,SO、NO、NH 和 H(5-17%)以及碱金属阳离子和 Cl(12-17%)在 1986-2019 年期间。在弗雷利堡,NADP 于 2011 年 10 月更换了采样器。对于 2002-2011 年,弗雷利堡的相对差异为正值,且与宾夕法尼亚州立大学的相对差异相似。对于 2012-2019 年,除 H 较高(高 23%)外,降水加权年平均浓度比 NADP 低 5-27%,除 H 外,其他所有离子的降水加权年平均浓度都比 NADP 低 5-27%,只有 H 较高(高 23%)。NADP 更换采样器对网络间偏差的影响最大。CAPMoN 网络在 1999-2001 年和 2016-2017 年同期进行的每日与每周测量值比较表明,每周测量值比每日测量值高 1-3%,SO、NO 和 NH;3-9%,Ca、Mg、Na 和 Cl;10-24%,K;H 则低 8-30%,以降水加权平均浓度计。因此,采样频率的差异并没有导致 CAPMoN 测量值的系统偏高。了解这些网络数据的偏差对于解释大陆尺度的沉降模型和跨界比较湿沉降趋势非常重要。