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首页> 外文期刊>Hydrology and Earth System Sciences >Coherent response of lakes in Ontario, Canada to reductions in sulphur deposition: the effects of climate on sulphate concentrations
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Coherent response of lakes in Ontario, Canada to reductions in sulphur deposition: the effects of climate on sulphate concentrations

机译:加拿大安大略湖对硫沉积减少的连贯响应:气候对硫酸盐浓度的影响

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摘要

Sulphate deposition in south-central Ontario declined between 1976 and 2000 by more than 50%, whereas lake sulphate (SO42–) concentrations decreased by, on average, only half as much. To investigate the factors that controlled this slower than expected response, the temporal patterns in lake SO42– concentrations were compared with patterns in both deposition and climate, since climate has a major influence on the hydrological cycle in this part of the continent. To do this, the temporal coherence in SO42– concentrations between 9 lake basins was estimated using the intraclass correlation from a repeated-measures analysis of variance and two subsets of lakes were found (six in one group, four in the other), each with lakes having synchronous patterns. One subset (4 lakes) included the 3 with the longest water replenishment times (>3.4 yr) which are expected to respond to decreases in SO42– deposition more slowly. However, the average pattern reflecting the temporal changes of each of the two subsets was very similar. The response of both subsets of lakes to the decreasing SO42– deposition over two decades was independent of the degree of acidification or sensitivity to acidification of the lakes. In a determination of which factors best predicted each of those two subsets’ SO42– time series, good predictive models were produced by regional/global-scale climate indices, specifically the Southern Oscillation Index (SOI) describing the El Ni?o Southern Oscillation (ENSO) and the North Atlantic Oscillation Index (NAOI), as well as by SO42– deposition indices. When the predictor variables were combined, models which described the long-term changes in lake SO42– concentration best included the SOI, the NAOI and SO42– deposition. Thus, large-scale climate factors play a major role in determining the response of aquatic systems to changes in SO42– deposition, perhaps through their influence on lake and/or catchment processes that effectively delay recovery. style="line-height: 20px;">Keywords: Atmospheric deposition, lake recovery, temporal trends, climate, temporal coherence
机译:1976年至2000年间,安大略省中南部的硫酸盐沉积下降了50%以上,而硫酸盐(SO 4 2 – )的浓度平均仅下降了一半尽可能多。为了研究控制这种慢于预期响应的因素,我们将SO 4 2-浓度的时空模式与沉积和气候模式进行了比较,因为气候具有对非洲大陆这部分的水文循环有重大影响。为此,使用类内相关性,通过方差和两个湖泊子集的重复测量分析,估算了9个湖流域之间SO 4 2-浓度的时间相干性被发现(一组六个,另一组四个),每个湖泊都有同步模式。一个子集(4个湖泊)包括三个补水时间最长(> 3.4年)的湖泊,这有望对SO 4 2-沉积速度的降低更为缓慢。但是,反映两个子集的每个时间变化的平均模式非常相似。湖泊的两个子集对SO 4 2-沉积在20年中减少的响应与湖泊的酸化程度或酸化敏感性无关。在确定哪些因素最能预测这两个子集的SO 4 2-时间序列中的每一个时,通过区域/全球尺度的气候指数,特别是产生了良好的预测模型描述厄尔尼诺南方涛动(ENSO)和北大西洋涛动指数(NAOI)的南方涛动指数(SOI),以及SO 4 2 – 沉积指数。结合预测变量后,描述湖泊SO 4 2-浓度长期变化的模型最好包括SOI,NAOI和SO 4 < / sub> 2 – 沉积。因此,大规模的气候因素可能在决定水生系统对SO 4 2-沉积变化的响应中起主要作用,可能是由于它们对湖泊和/或湖泊的影响。集水过程有效地延迟了恢复。 style =“ line-height:20px;”> 关键字:大气沉积,湖泊恢复,时间趋势,气候,时间连贯性

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