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Uncertainties in Sandy Shorelines Evolution under the Bruun Rule Assumption

机译:Bruun规则假设下桑迪海岸线演变的不确定性

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In the current practice of sandy shoreline change assessments, the local sedimentary budget is evaluated using the sediment balance equation, that is, by summing the contributions of longshore and cross-shore processes. The contribution of future sea-level-rise induced by climate change is usually obtained using the Bruun rule, which assumes that the shoreline retreat is equal to the change of sea-level divided by the slope of the upper shoreface. However, it remains unsure that this approach is appropriate to account for the impacts of future sea-level rise. This is due to the lack of relevant observations to validate the Bruun rule under the expected sea-level rise rates. To address this issue, this article estimates the coastal settings and period of time under which the use of the Bruun rule could be (in)validated, in the case of wave-exposed gently-sloping sandy beaches. Using the sedimentary budgets of Stive (2004) and probabilistic sea-level rise scenarios based on IPCC, we provide shoreline change projections that account for all uncertain hydrosedimentary processes affecting idealized coasts (impacts of sea-level rise, storms and other cross-shore and longshore processes). We evaluate the relative importance of each source of uncertainties in the sediment balance equation using a global sensitivity analysis. For scenario RCP 6.0 and 8.5 and in the absence of coastal defences, the model predicts a perceivable shift toward generalized beach erosion by the middle of the 21st century. In contrast, the model predictions are unlikely to differ from the current situation in case of scenario RCP 2.6. Finally, the contribution of sea-level rise and climate change scenarios to sandy shoreline change projections uncertainties increases with time during the 21st century. Our results have three primary implications for coastal settings similar to those provided described in Stive (2004) : first, the validation of the Bruun rule will not necessarily be possible under scenario RCP 2.6. Second, even if the Bruun rule is assumed valid, the uncertainties around average values are large. Finally, despite these uncertainties, the Bruun rule predicts rapid shoreline retreat of sandy coasts during the second-half of the 21st century without strong réductions of greenhouse gas emissions.
机译:在目前的沙质海岸线变化评估实践中,使用沉积物平衡方程式(即通过将长岸和跨岸过程的贡献相加)来评估局部沉积物预算。气候变化引起的未来海平面上升的贡献通常是使用布鲁恩法则获得的,该法则假设海岸线的撤退等于海平面的变化除以上岸面的坡度。但是,仍然不确定该方法是否适合解决未来海平面上升的影响。这是由于缺乏相关的观察结果来验证预期海平面上升速率下的布鲁恩规则。为解决此问题,本文估计了在波浪暴露且缓坡的沙滩情况下,可以(不)验证使用(不)使用Bruun规则的沿海环境和时间段。使用Stive(2004)的沉积预算和基于IPCC的概率海平面上升方案,我们提供了海岸线变化预测,这些变化说明了影响理想海岸的所有不确定的水沉积过程(海平面上升,风暴和其他跨海岸和长岸过程)。我们使用全局敏感性分析评估沉积物平衡方程中每个不确定性源的相对重要性。对于情景RCP 6.0和8.5,并且在没有沿海防御的情况下,该模型预测,到21世纪中叶,可感知的转向普遍的海滩侵蚀。相反,在场景RCP 2.6的情况下,模型预测不太可能与当前情况有所不同。最后,在21世纪,海平面上升和气候变化情景对沙质海岸线变化预测不确定性的贡献随时间增加。我们的研究结果对沿海环境有三个主要影响,类似于Stive(2004)中所述:首先,在RCP 2.6情景下,对Bruun规则的验证不一定是可能的。其次,即使假定布鲁因规则有效,平均值周围的不确定性也很大。最后,尽管存在这些不确定性,但布劳恩规则仍预测,在21世纪下半叶,沙质海岸的海岸线将快速退缩,而温室气体的排放量不会大量减少。

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