利用oceanansat -2散射计风在北印度洋进行的WAM和WAVEWATCH-III相互比较研究

J. Swain, P. Umesh, AN Balchand
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引用次数: 10

摘要

本文介绍了在1°× 1°(纬度×经度)网格分辨率下,使用第三代模式WAM和WAVEWATCH-III进行的北印度洋波浪预报的相互比较,通过模式结果的相互比较,首次对它们的相对性能进行了评价。本文分析了利用Oceansat-2散射计风模拟得到的后投波参数,如有效波高、平均波周期和膨胀波高,以了解与印度洋单个模式输出相关的质量和变率。对四个不同病例(2010年1月和6月,以及2011年1月和6月)进行了WAM和WAVEWATCH-III相互比较研究。通过广泛而稳健的统计误差分析,对这两种模型的相对性能进行了比较研究。基于对模式结果的定性和定量评估,本研究清楚地表明,WAM和WAVEWATCH-III在使用Oceansat-2散射计风的共同模式域中表现良好,它们可以自信地用于北印度洋的长期后投,这将对处理各种沿海/近海活动的大多数用户社区非常有用。该研究还建议,最好考虑在北印度洋的深海和沿海水域进行现有的长期波浪测量,以进一步验证和比较WAM和WAVEWATCH-III。
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WAM and WAVEWATCH-III intercomparison studies in the North Indian Ocean using Oceansat-2 Scatterometer winds
This paper presents the intercomparison of wave hindcasts using the third-generation models WAM and WAVEWATCH-III for the North Indian Ocean over 1° × 1° (latitude × longitude) grid resolutions, which reveals the first assessment of their relative performance through intercomparison of the model results. Hindcast wave parameters such as significant wave height, mean wave period, and swell wave height obtained from the simulations using Oceansat-2 scatterometer winds are analyzed to understand the quality and variability associated with the individual model outputs in the Indian Ocean. WAM and WAVEWATCH-III intercomparison studies are carried out for four different cases (January and June 2010, and January and June 2011). A comparative study of the relative performances of these two models is evaluated through extensive and robust statistical error analysis. Based on both qualitative and quantitative assessment of the model results, this study clearly indicates that both WAM and WAVEWATCH-III performed well in the common model domain using Oceansat-2 scatterometer winds, and they can be confidently used for long-term hindcasting in the North Indian Ocean, which will be very useful for most of the user community dealing with various coastal/offshore activities. The study also suggests that it would be preferable to consider available long-term wave measurements both in deep and coastal waters of the North Indian Ocean to validate and intercompare WAM and WAVEWATCH-III further.
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