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Modelling the future impacts of climate and land-use change on suspended sediment transport in the River Thames (UK)

机译:模拟气候和土地利用变化对泰晤士河(英国)悬浮泥沙输移的未来影响

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摘要

The effects of climate change and variability on river flows have been widely studied. However the impacts of such changes on sediment transport have received comparatively little attention. In part this is because modelling sediment production and transport processes introduces additional uncertainty, but it also results from the fact that, alongside the climate change signal, there have been and are projected to be significant changes in land cover which strongly affect sediment-related processes. Here we assess the impact of a range of climatic variations and land covers on the River Thames catchment (UK). We first calculate a response of the system to climatic stressors (average precipitation, average temperature and increase in extreme precipitation) and land-cover stressors (change in the extent of arable land). To do this we use an ensemble of INCA hydrological and sediment behavioural models. The resulting system response, which reveals the nature of interactions between the driving factors, is then compared with climate projections originating from the UKCP09 assessment (UK Climate Projections 2009) to evaluate the likelihood of the range of projected outcomes. The results show that climate and land cover each exert an individual control on sediment transport. Their effects vary depending on the land use and on the level of projected climate change. The suspended sediment yield of the River Thames in its lowermost reach is expected to change by −4% (−16% to +13%, confidence interval, p = 0.95) under the A1FI emission scenario for the 2030s, although these figures could be substantially altered by an increase in extreme precipitation, which could raise the suspended sediment yield up to an additional +10%. A 70% increase in the extension of the arable land is projected to increase sediment yield by around 12% in the lowland reaches. A 50% reduction is projected to decrease sediment yield by around 13%.
机译:气候变化和多变性对河流流量的影响已得到广泛研究。但是,这种变化对泥沙输送的影响很少受到关注。在某种程度上,这是因为对沉积物生产和运输过程进行建模会带来额外的不确定性,但这还源于以下事实:与气候变化信号一起,已经并且预计将发生显着的土地覆盖变化,这将严重影响与沉积物相关的过程。在这里,我们评估了各种气候变化和土地覆盖对泰晤士河集水区(英国)的影响。我们首先计算系统对气候压力源(平均降水,平均温度和极端降水增加)和土地覆盖压力源(耕地范围的变化)的响应。为此,我们使用INCA水文和沉积物行为模型的集合。然后将得出的系统响应(揭示驱动因素之间相互作用的性质)与源自UKCP09评估的气候预测(UK Climate Projections 2009)进行比较,以评估预期结果范围的可能性。结果表明,气候和土地覆盖均对沉积物的运移具有独立的控制作用。其影响取决于土地用途和预计的气候变化水平。在2030年代A1FI排放情景下,泰晤士河最下游的悬浮泥沙产量预计将变化-4%(− 16%至+ 13%,置信区间,p = 0.95),尽管这些数字可能是极端降水的增加会极大地改变这种状况,这可能会使悬浮泥沙的产生增加多达+ 10%。预计可耕地扩展70%将使低地河段的泥沙产量增加约12%。预计减少50%会使沉积物产量减少约13%。

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