在Welander模型中对深度解/深度合振荡的详细分析
John Bailie1, Henk A Dijkstra2, Bernd Krauskopf1
1Department of Mathematics, The University of Auckland, Private Bag 92019, Auckland 1010, New Zealand.
Chaos (Woodbury, N.Y.)
|July 14, 2025
概括
韦兰德模型显示了深水混合和脱之间的振荡. 顺切换功能揭示了新的振荡类型和由淡水流入驱动的过渡,需要更快的切换来实现持续的深度解.
科学领域:
- 海洋学 海洋学 海洋学
- 气候科学 气候科学
- 地质物理学 地质物理学
背景情况:
- 韦兰德概念模型模拟了海洋温度和盐度的演变.
- 它使用两个垂直堆叠的盒子,代表表面和深水.
- 相互作用通过扩散和对流调整发生.
研究的目的:
- 为了全面研究Welander模型中的振荡,以平稳的,非瞬间切换.
- 根据扩散和对流混合相识别和描述不同的振荡类型.
- 为了研究淡水逐渐涌入对振荡过渡的影响.
主要方法:
- 在Welander模型中使用了流的,非即时的切换功能.
- 分析参数空间以确定不同振荡类型的区域.
- 模拟了淡水逐渐涌入对模型动态的影响.
主要成果:
- 根据混合阶段确定了四种不同的振荡类型.
- 证实了威兰德特有的深度解振荡仍然存在,但需要更快的切换.
- 由淡水流入引起的振荡类型之间的过渡证明.
结论:
- 顺切换函数在韦兰德模型中揭示了复杂的振荡行为.
- 持续的深度解振荡需要快速切换动态.
- 淡水强迫可以动态地改变海洋混合模式.
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