印度洋风海与涌浪研究进展综述

P. V. Ethamony, R. Rashmi, S. Samiksha, V. M. Aboobacker
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引用次数: 11

摘要

分析了印度西海岸几个地点的风浪数据和波浪模型结果,研究了不同季节深岸和近岸地区的波浪特征。在天气晴朗的季节,我们可以观察到明显系统的波高和波周期的日变化,特别是随着当地风速的增加,波高和波周期同时增加和减少。这是由于海风系统产生的风海与先前存在的海浪叠加造成的。在西南季风季节,阿拉伯海的涌浪主要来自西南方向,而在季风前和季风后,阿拉伯海的涌浪主要来自西南/西南偏南和西北方向。夏马尔事件发生的北西向巨浪表现出浪高增加、浪高周期缩短、风海和巨浪有共同的传播方向(西北)等特点。此外,在400s产生的涌浪在北印度洋传播,进入孟加拉湾而不影响阿拉伯海。细分辨率风(如MM5或WRF)对于了解陆海风系统对沿海地区风海产生的影响是必要的。在这里,我们回顾了最近我们利用实测波浪数据和模型结果在印度洋和沿海地区进行的关于风海和海浪的工作。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Recent Studies on Wind Seas and Swells in the Indian Ocean: A Review
Winds and waves data measured at a few locations along the west coast of India as well as wave model results were analysed to study the wave characteristics in the deep as well as nearshore regions during different seasons. During fair weather season, we can observe distinct and systematic diurnal variation in wave height and wave period, especially, simultaneous increase in wave height and decrease in wave period with increase in local wind speed. This is due to superimposition of wind seas generated by the sea breeze system with the pre-existing swells. The swells observed in the Arabian Sea are from SW direction during SW monsoon season and from SW/SSW and NW directions during both pre-monsoon and post-monsoon seasons. The NW swells which occur during Shamal events show distinct characteristics such as an increase in wave height, decrease in swell period and a common propagation direction (northwest) for wind seas and swells. Also the swells generated at 400 S, propagate in the north Indian Ocean, and enter the Bay of Bengal without affecting the Arabian Sea. Fine resolution winds (say, MM5 or WRF) are necessary to understand the effect of land-sea breeze system on wind-sea generation in the coastal regions. Here, we review the recent work on wind seas and swells in the Indian Ocean and coastal regions that we have carried out using measured wave data and model results.
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