沿海线对海平面上升的反应根据平衡的海形状
Pau Luque1, Lluís Gómez-Pujol2, Francesca Ribas3
1Mediterranean Institute for Advanced Studies (IMEDEA), Spanish National Research Council - University of the Balearic Islands (CSIC-UIB), Esporles, Spain. pau.luque@uib.es.
Scientific reports
|September 22, 2023
概括
沿海侵蚀模型必须考虑整个出现的海,而不仅仅是淹没的区域,以准确预测沿海变化. 使用瞬间强迫条件显著降低了海岸线演变预测的不确定性,特别是在狭窄的海上.
科学领域:
- 沿海的地形形态.
- 靠近海岸的水力动力学.
- 形态动力学建模模型
背景情况:
- 海岸线位置是沙状态和对海平面上升等强迫因素的反应的关键指标.
- 海岸线的变化是各种时间尺度上复杂的合水力动力学和形态动力学过程的结果.
- 现有的十年级海岸线演变模型通常通过使用平衡海配置文件来简化.
研究的目的:
- 根据平衡海形状,推导出海岸线演变的一般方程.
- 为了评估海平面上升,波浪和高频海平面强迫下的海岸线变化.
- 将衍生模型与现有的分析和动态模型进行比较.
主要方法:
- 使用平衡海配置文件开发海岸线演变的一般方程.
- 基于常见假设的模型细分化.
- 与分析平衡沙形状模型和动态沉积物运输模型进行比较.
主要成果:
- 考虑到出现的海区域受到海洋强迫的影响至关重要,而不仅仅是淹没的部分.
- 海岸线衰退率在狭窄的海上可能有所不同,海上强迫影响了整个空面.
- 布鲁恩法则适用,但对活动型的陆地边界定义非常敏感.
结论:
- 衍生模型强调了将新出现的海纳入海岸线演变评估的重要性.
- 即时强迫条件大大降低了与定义主动配置界限相关的不确定性.
- 准确的海岸线演变预测需要仔细考虑强迫条件和海几何形状.
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