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Predicted Wave Climate for the UK: towards an Integrated Model of Coastal Impacts of Climate Change

机译:英国的预测海浪气候:建立气候变化对海岸影响的综合模型

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摘要

The effect of global climate change on the wave climate of the coastal regions of the UK is investigated. A state of the art third generation wave model is used to predict changes in wave climate in the North East Atlantic and UK coastal waters. The driving meteorological data is provided by global and regional climate models, driven by different future greenhouse gas emissions scenarios. Present day wave climates are validated against a previous hindcast, which has been calibrated with wave observations, and good agreement is found in regions of interest. These studies downscale the affect of global climate changes on wave climate to a previously unresolved scale. Ouput of these wave climate predictions are to be used in a regional Coastal Simulator manged by the Tyndall Centre for Climate Change Research. The Coastal Simulator is a framework of integrated hydrodynamic, morphological and socio-economic models that provides predictions of the increased risks of coastal flooding and cliff erosion on the East Anglia coastline. The drivers of increased risks are sea-level rise and increased storm surges and waves in possible future climate scenarios. On a large scale, for the range of future climate scenarios, strong positive changes in significant wave height are predicted in the North East Atlantic and South West of the UK. On the regional scale of the Southern North Sea the spatial pattern of changes in wave height varies considerably with possible future scenario, but positive changes in the mean and high percentiles of wave height are predicted off-shore from the particular region of interest on the East Anglia coastline.
机译:研究了全球气候变化对英国沿海地区波浪气候的影响。最先进的第三代波浪模型用于预测东北大西洋和英国沿海水域的波浪气候变化。驱动的气象数据由全球和区域气候模型提供,这些模型由未来不同的温室气体排放情景驱动。目前的海浪气候已根据先前的后兆进行了验证,后者已经通过海浪观测进行了校准,并且在感兴趣的地区发现了很好的一致性。这些研究将全球气候变化对海浪气候的影响降低到了以前无法解决的规模。这些波浪气候预测的结果将在廷德尔气候变化研究中心管理的区域沿海模拟机中使用。沿海模拟器是综合的水动力,形态学和社会经济模型的框架,该模型提供了对东安格利亚海岸线上沿海洪水和悬崖侵蚀风险增加的预测。风险增加的驱动因素是海平面上升以及未来可能的气候情景中风暴潮和海浪的增加。在未来的气候情景范围内,预计在英国的东北大西洋和西南地区,在重要的波高上会有很大的积极变化。在南北海区域尺度上,海浪高度的空间格局随未来的可能情况而有很大变化,但预计离海浪较远的东部特定海域的海浪平均值和高百分位数将出现正向变化英吉利海岸线。

著录项

  • 来源
    《Estuarine and coastal modeling》|2007年|393-406|共14页
  • 会议地点 Newport RI(US);Newport RI(US)
  • 作者单位

    Proudman Oceanographic Laboratory. 6 Brownlow Street. Liverpool, L3 5DA;

    Proudman Oceanographic Laboratory. 6 Brownlow Street. Liverpool, L3 5DA;

    Met Office Hadley Centre (Reading Unit);

    University of Manchester Tyndall Centre for Climate Change Research;

    University of Manchester Tyndall Centre for Climate Change Research;

    Tyndall Centre for Climate Change Research University of Southampton;

    Tyndall Centre for Climate Change Research University of Southampton;

    Tyndall Centre for Climate Change Research University of East Anglia;

    Tyndall Centre for Climate Change Research University of Newcastle upon Tyne;

    Tyndall Centre for Climate Change Research University of East Anglia;

    Tyndall Centre for Climate Change Research University of Southampton;

  • 会议组织
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 海洋工程;
  • 关键词

  • 入库时间 2022-08-26 13:59:55

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