沉积物运输和形态演变对具有不同特征的风暴的反应
Can Wang1, Gang Yang2, Chunhui Li2
1School of Geographical Sciences, Nanjing University of Information Science and Technology, Nanjing 210044, China.
The Science of the total environment
|June 19, 2024
概括
沿海风暴事件导致复杂的沉积物变化. 一个新的模型揭示了潮和重力,受风和海浪的影响,控制沉积物运输和风暴期间的海底侵蚀/沉积.
科学领域:
- 沿海的地形形态.
- 海洋学 海洋学 海洋学
- 沉积物动态 沉积物的动态
背景情况:
- 风暴事件通过沉积物再悬浮和运输显著改变沿海地形.
- 了解风暴期间这些复杂的沉积过程至关重要,但仍然不完整.
研究的目的:
- 通过结合模型研究沿海动态过程对极端风暴事件的反应.
- 分析风暴期间驱动沉积物运输和形态变化的机制.
主要方法:
- 开发和验证一个合波电流沉积物模型.
- 数字实验模拟风暴条件 (台风Wipha) 和美好天气场景.
- 分析潮抽水效应和沉积物流动上的重力循环.
主要成果:
- 模拟的长海岸沉积物运输在风暴期间由风引起的波浪增强.
- 确定了两种典型的沉积物动态反应模式,它们由潮抽和引力循环控制.
- 引力循环 (T6) 起到了关键作用,常常对抗主导风暴.
- 强风诱导水柱分层,导致横岸沉积物运输和海底侵蚀/沉积.
- 陆上风对沉积物过程产生了更大的影响.
结论:
- 开发的模型准确地模拟了在暴风雨和晴朗天气条件下的沿海沉积过程.
- 风暴诱导的沉积物运输是由潮,波浪和风力驱动的力量的组合控制的.
- 引力循环和风的影响是风暴期间沿海形态变化的关键因素.
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