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The British river of the future: how climate change and human activity might affect two contrasting river ecosystems in England

机译:未来的英国河流:气候变化和人类活动如何影响英格兰两个截然相反的河流生态系统

摘要

The possible effects of changing climate on a southern and a north-eastern English river (the Thames and the Yorkshire Ouse, respectively) were examined in relation to water and ecological quality throughout the food web. The CLASSIC hydrological model, driven by output from the Hadley Centre climate model (HadCM3), based on IPCC low and high CO2 emission scenarios for 2080 were used as the basis for the analysis. Compared to current conditions, the CLASSIC model predicted lower flows for both rivers, in all seasons except winter. Such an outcome would lead to longer residence times (by up to a month in the Thames), with nutrient, organic and biological contaminant concentrations elevated by 70–100% pro-rata, assuming sewage treatment effectiveness remains unchanged. Greater opportunities for phytoplankton growth will arise, and this may be significant in the Thames. Warmer winters and milder springs will favour riverine birds and increase the recruitment of many coarse fish species. However, warm, slow-flowing, shallower water would increase the incidence of fish diseases. These changing conditions would make southern UK rivers in general a less favourable habitat for some species of fish, such as the Atlantic salmon (Salmo salar). Accidental or deliberate, introductions of alien macrophytes and fish may change the range of species in the rivers. In some areas, it is possible that a concurrence of different pressures may give rise to the temporary loss of ecosystem services, such as providing acceptable quality water for humans and industry. An increasing demand for water in southern England due to an expanding population, a possibly reduced flow due to climate change, together with the Water Framework Directive obligation to maintain water quality, will put extreme pressure on river ecosystems, such as the Thames.
机译:研究了气候变化对英格兰南部和东北部河流(分别为泰晤士河和约克郡乌斯河)的可能影响,并与整个食物网中的水和生态质量相关。由哈德利中心气候模型(HadCM3)的输出驱动的CLASSIC水文模型基于IPCC 2080年的低和高CO2排放情景作为分析的基础。与当前条件相比,CLASSIC模型预测除冬季以外的所有季节,两条河流的流量都较低。如果污水处理的效果保持不变,那么这样的结果将导致更长的停留时间(在泰晤士河中最多可停留一个月),并且营养,有机和生物污染物的浓度按比例增加70-100%。浮游植物的增长机会将会增加,这在泰晤士河可能很重要。温暖的冬天和温和的春天将有利于河禽,并增加了许多粗养鱼类的数量。但是,温暖,流动缓慢的浅水会增加鱼类疾病的发病率。这些变化的条件将使英国南部的河流总体上不适合某些鱼类的栖息地,例如大西洋鲑鱼(Salmo salar)。偶然或故意引入外来植物和鱼类可能会改变河流中物种的范围。在某些地区,不同压力的并发可能会导致生态系统服务的暂时丧失,例如为人类和工业提供可接受的优质水。由于人口增加,英格兰南部对水的需求不断增加,由于气候变化可能导致水流量减少,再加上《水框架指令》规定的维持水质的义务,将对泰晤士河等河流生态系统造成极大压力。

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