评估模型模拟的热带气旋对生物地球化学参数的反应,使用在阿拉伯海的浮动观测进行分析
V P Thangaprakash1, M S Girishkumar2, N Sureshkumar2
1Indian National Centre for Ocean Information Services (INCOIS), Hyderabad, 500090, India. thangaprakash.vp@incois.gov.in.
Scientific reports
|July 2, 2025
概括
热带气旋Ockhi显著加深了混合层,增加了阿拉伯海的叶绿素和初级生产力. 虽然区域海洋模型系统 (ROMS) 捕获了趋势,但它显示了叶绿素和溶氧模拟时间和大小的差异.
科学领域:
- 海洋生物地质化学海洋生物地质化学
- 物理海洋学 物理海洋学
- 数字建模 数字建模
背景情况:
- 热带气旋 (TCs) 对海洋物理和生物地球化学有着深刻的影响.
- 了解这些影响对于预测海洋生态系统反应至关重要.
- 生物地化学Argo浮标为模型验证提供了有价值的现场数据.
研究的目的:
- 评估区域海洋模型系统 (ROMS) 结合生物物理模型的能力.
- 模拟TC Ockhi期间的物理和生物地球化学状态.
- 为了将模型输出与生物地球化学Argo浮动测量进行比较.
主要方法:
- 利用了来自生物地球化学阿戈浮体 (A浮体) 的数据.
- 采用区域海洋模型系统 (ROMS) 进行合生物物理模拟.
- 分析了混合层深度,叶绿素,溶解氧和初级生产力的变化.
主要成果:
- TC Ockhi将混合层深化到49米 (观察到影响高达95米).
- 地表附近的叶绿素在TC后显著增加,提高了初级生产力.
- 罗姆斯模型通常捕获时间趋势,但高估了叶绿素和DO,在峰值叶绿素反应的时间差异.
结论:
- 结合的ROMS模型显示了模拟TC驱动的海洋学变化的潜力.
- 模型性能需要改进,特别是在捕捉生物地化学反应的精确时间和大小方面.
- 来自A浮体的现场数据对于验证和改进这些模型至关重要.
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