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Impacts of Droughts and Acidic Deposition on Long-Term Surface Water Dissolved Organic Carbon Concentrations in Upland Catchments in Wales

机译:干旱和酸性沉积对威尔士高地集水区长期水分溶解有机碳浓度的影响

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Concerns have been raised about rising trends in surface water dissolved organic carbon (DOC) concentrations in UK upland catchments over the past decades. Several mechanisms have been proposed to explain these trends, including changes in climate and declines in sulphate deposition across Europe. Drier summers and wetter winters are projected in the UK, and there is an increasing interest in whether the rising trends of DOC would be continued or stabilised. In this paper, the INCA (INtegrated CAtchment) water quality model was applied to the upland catchment of the River Severn at Plynlimon in Wales and used to simulate the effects of both climate and sulphate deposition on surface water DOC concentrations. We introduced new parameter sets of INCA to explain enzymatic latch effect in peatlands during droughts. The model was able to simulate recent past (1995-2013) rising trends in DOC in Plynlimon. Climatic projections were employed to estimate the future trends on DOC in the uplands and to consider potential impacts on catchment management. The model was run with climatic scenarios generated using the weather@home2 climate modelling platform and with sulphate deposition scenarios from the European Monitoring and Evaluation Programme (EMEP) for 1975-2100. The modelling results show that the rising DOC trends are likely to continue in the near future (2020-2049) and the level of DOC concentrations is projected to stabilise in the far future (2070-2099). However, in the far future, the seasonal patterns of DOC concentrations will change, with a post-drought DOC surge in autumn months.
机译:的担忧已经提出了关于在表面水中的趋势上升溶解的有机碳(DOC)的浓度在英国高地集水在过去几十年。一些机制已经提出来解释这些趋势,包括气候变化在欧洲硫酸盐沉积下降。干燥的夏季多雨,冬季预计在英国,并且在DOC的上升趋势是否会持续或稳定的兴趣越来越大。在本文中,INCA(集成集水)水质模型在威尔士在Plynlimon施加到河Severn的高地集水区和用于模拟气候和硫酸盐沉积于表面的水浓度DOC的效果。我们引入了新的参数集INCA的干旱期间解释放量酶锁存器的作用。该模型能够模拟最近(1995年至2013年)上升趋势中DOC Plynlimon。气候预测是用来估计在高地DOC未来的发展趋势,并考虑对流域管理的潜在影响。该模型是利用天气气候产生的场景运行@ HOME2气候建模平台,并与来自欧洲监测和评估方案而得到确证为1975至2100年硫酸盐沉积的情景。模拟结果表明,上升趋势DOC可能会继续在不久的将来(2020年至2049年)和DOC浓度的水平,预计在不远的将来(2070至2099年)来稳定。然而,在不远的将来,DOC浓度的季节性模式将发生变化,在秋天个月干旱后DOC激增。

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