破浪产生的气泡羽流动力学

D. Pelaez-Zapata, V. Pakrashi, Frédéric Dias
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引用次数: 0

摘要

气泡羽流通过影响海气交换、气溶胶生成、海洋碳和营养物循环调节以及上层海洋垂直结构等过程,在海气界面发挥着重要作用。利用在爱尔兰西海岸收集的声学多普勒海流剖面仪(ADCP)数据,我们研究了气泡羽流的动态及其与海况变量的关系。我们特别描述了气泡羽流的垂直延伸、持续时间和周期模式。我们确定了气泡平均穿透深度与风速之间的幂律关系,这与之前的研究结果一致。此外,研究还揭示了白化覆盖率与观测到的声学体积反向散射强度之间的重要关联,强调了破浪在气泡羽流产生过程中的作用。气泡羽流深度的概率分布形状显示,在风速较高时,气泡夹带事件会变得更强、更有组织。此外,我们还发现,更深的气泡羽流与湍流Langmuir数Lat∼ 0.3有关,突出了Langmuir环流对气泡羽流的传输和加深的潜在作用。这些结果有助于更好地理解海浪、风和气泡羽流之间复杂的相互作用,为改进预测模型和加深我们对海气相互作用的理解提供了宝贵的见解。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Dynamics of bubble plumes produced by breaking waves
Bubble plumes play a significant role in the air-sea interface by influencing processes such as air-sea gas exchange, aerosol production, modulation of oceanic carbon and nutrient cycles, and the vertical structure of the upper ocean. Using Acoustic Doppler Current Profiler (ADCP) data collected off the west coast of Ireland, we investigate the dynamics of bubble plumes and their relationship with sea state variables. In particular, we describe the patterns of bubble plumes vertical extension, duration and periodicity. We establish a power-law relationship between the average bubble penetration depth and wind speed, consistent with previous findings. Additionally, the study reveals a significant association between whitecapping coverage and observed acoustic volume backscatter intensity, underscoring the role of wave breaking in bubble plume generation. The shape of the probability distribution of bubble plume depths reveals a transition towards stronger and more organised bubble entrainment events during higher wind speeds. Furthermore, we show that deeper bubble plumes are associated with turbulent Langmuir number Lat∼ 0.3, highlighting the potential role of Langmuir circulation on the transport and deepening of bubble plumes. These results contribute to a better understanding of the complex interactions between ocean waves, wind, and bubble plumes, providing valuable insights for improving predictive models and enhancing our understanding of air-sea interactions.
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