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Long-term monitoring of precipitation chemistry in the U.S.: Insights into changes and condition

机译:在美国的降水化学长期监测:洞察变化和条件

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Continuous monitoring of precipitation chemistry began at the Hubbard Brook Experimental Forest, NH in June 1963, and it was there that acid rain was discovered in North America. Some independent monitoring of precipitation chemistry in central New York was done in 1970-1971. The MAP3S network (Charlottesville, VA, Ithaca, NY, Penn State, PA, Whiteface Mt., NY) began in 1976 and became part of the National Atmospheric Deposition Program (NADP) in 1992. Using data from these long-term sites, and other published information, we show the status and temporal change of precipitation chemistry in the northeastern U.S. from 1963 to present. Combining records from all stations and networks gave better insights into the status and temporal trends of precipitation chemistry for the region particularly as detailed regional maps could be constructed from these data. Early maps of predicted pH (1955-56 and 1965-66) and individually measured pH values (1975-76), as well as cartoons provided important visual information about the occurrence and spread of acid rain in the northeastern U.S. These indicators of changing atmospheric chemistry were key in initiating federal policy necessary for improving air quality and for reducing atmospheric pollutant loading, which had led to acid rain in this area, starting in the 1950s. Analyzing combined records from Hubbard Brook and the 5 longest operating MAP3S/AIRMoN sites (IL11, NY67, DE02, PA15 and TN00) with a random coefficient model showed overall declines in annual concentrations of H+, SO42+ and NO3- from 1981 to 2017 of 85%, 80% and 66%, respectively. Calcium concentration declined by 14% and NH4+ showed no change during this period. Dry deposition of sulfur, NO3- and Ca2+ measured at co-located Clean Air Status and Trends Network (CASTNET) sites showed declines of 87%, 64% and 1%, respectively, during 2000-2017. As precipitation and air chemistry networks expanded to include the entire US (and Canada), dramatic improvements in precipitation chemistry nationwide, brought about by federal, clean air legislation, have been clearly documented.
机译:1963年6月,哈伯德溪实验森林,北美洲,北美发现了哈伯德·溪实验森林的持续监测降水化学。纽约中部的沉淀化学的一些独立监测于1970年至1971年完成。 Map3s网络(Charlottesville,VA,Ithaca,Ny,Penn State,Pa,Whiteface Mt.,NY)于1976年开始于1992年成为国家大气沉积计划(NADP)的一部分。使用来自这些长期站点的数据,和其他公布的信息,我们从1963年展示了美国东北部的降水化学的现状和时间变化。组合所有站和网络的记录对该地区的降水化学的状态和时间趋势更好地见解,特别是因为可以从这些数据构成详细的区域地图。预测pH(1955-56和1965-66)的早期地图和单独测量的pH值(1975-76),以及漫画提供了关于美国东北部酸雨的发生和传播的重要视觉信息,这些指标改变了大气变化了大气化学是启动提高空气质量所必需的联邦政策以及减少大气污染物载荷所必需的关键,这在20世纪50年代开始导致该地区的酸雨。分析来自Hubbard Brook的组合记录和具有随机系数模型的Hubbard Brook和5个最长的操作MAP3S / AIRMON网站(IL11,NY67,DE02,PA15和TN00)表现出每年浓度的H +,SO42 +和NO3--- 2017年的总体下降85 %,80%和66%。钙浓度下降14%,NH4 +在此期间没有变化。在共同定位的清洁空气状态和趋势网络(FastNet)地点测量的硫沉积,No3-和Ca2 +分别在2000-2017期间显示出87%,64%和<1%的下降。随着降水和空气化学网络扩大到包括整个美国(加拿大),通过联邦,清洁空气立法所带来的全国沉淀化学的戏剧性改善,已明确记录。

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