...
首页> 外文期刊>Climatic Change >The morphological response of large tidal inlet/basin systems to relative sea level rise
【24h】

The morphological response of large tidal inlet/basin systems to relative sea level rise

机译:大型潮汐入口/盆地系统对相对海平面上升的形态响应

获取原文
获取原文并翻译 | 示例
           

摘要

The morphodynamic response of large tidal inlet/basin systems to future relative sea level rise (RSLR), incorporating both Eustatic sea level rise and local land subsidence effects, is qualitatively investigated using the state-of-the-art Delft3D numerical model and the Realistic analogue modelling philosophy. The modelling approach is implemented on a highly schematised morphology representing a typical large inlet/basin system located on the Dutch Wadden Sea (Ameland Inlet) over a 110-year study period. Three different RSLR Scenarios are considered: (a) No RSLR, (b) IPCC lower sea level rise (SLR) projection (0.2 m SLR by 2100 compared to 1990) and land subsidence, and (c) IPCC higher SLR projection (0.7 m SLR by 2100 compared to 1990) and land subsidence. Model results indicate that, for the 110-year study duration, the existing flood dominance of the system will increase with increasing rates of RSLR causing the ebb-tidal delta to erode and the basin to accrete. The rates of erosion/accretion are positively correlated with the rate of RSLR. Under the No RSLR condition, the tidal flats continue to develop while under the high RSLR scenario tidal flats eventually drown, implying that under this condition the system may degenerate into a tidal lagoon within the next 110 years. The tidal flats are stable under the low RSLR scenario implying that, at least for the next 100 years, this may be the critical RSLR condition for the maintenance of the system. Essentially the results of this study indicate that, as the Eustatic SLR is likely to be greater than the apparently critical rise of 0.2 m (by 2100 compared to 1990), the tidal flats in these systems will at least diminish. In the worst, but not unlikely, scenario that the Eustatic SLR is as high as the IPCC higher projections (0.7 m by 2100), the tidal flats may completely disappear. In either case, the associated environmental and socio-economic impacts will be massive. Therefore, more research focusing on the quantification of the physical and socio-economic impacts of RSLR on these systems is urgently needed to enable the development of effective and timely adaptation strategies.
机译:使用最新的Delft3D数值模型和实际方法,定性地研究了潮汐入口/流域系统对未来相对海平面上升(RSLR)的形态动力学响应,并结合了静态海平面上升和局部陆地沉降效应。模拟建模理念。该建模方法是在高度图解的形态学上实施的,该形态学代表了110年研究期间位于荷兰瓦登海(阿默兰湾)上的典型大型进水口/流域系统。考虑了三种不同的RSLR方案:(a)无RSLR,(b)IPCC低海平面上升(SLR)预测(到2100年与1990年相比,SLR为0.2 m)和地面沉降,以及(c)IPCC高SLR预测(0.7 m与1990年相比,到2100年实现了SLR)和地面沉降。模型结果表明,在为期110年的研究期间,该系统现有的洪水优势将随着RSLR速率的增加而增加,从而引起潮汐三角洲侵蚀和盆地增生。侵蚀/增生的速率与RSLR的速率呈正相关。在无RSLR条件下,滩涂继续发展,而在高RSLR情况下,最终淹没了滩涂,这意味着在这种情况下,系统可能在接下来的110年内退化为潮汐泻湖。在低RSLR情况下,潮滩是稳定的,这意味着至少在接下来的100年里,这可能是RSLR维护系统的关键条件。本质上,这项研究的结果表明,由于Eustatic SLR可能大于0.2 m的明显上升幅度(与1990年相比,上升了2100),因此这些系统中的潮汐平面至少会减小。在最坏但并非不可能的情况下,Eurstatic SLR达到IPCC更高的预测(到2100年为0.7 m)时,潮汐平面可能会完全消失。无论哪种情况,相关的环境和社会经济影响都是巨大的。因此,迫切需要进行更多的研究,重点是对RSLR对这些系统的物理和社会经济影响进行量化,以制定有效,及时的适应策略。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号