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Spectral separation of wind sea and swell based on buoy observations

机译:基于浮标观测的风海和膨胀的光谱分离

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Coexistence of swells from distant sources and wind seas generated by local wind field results in complex surface wave condition. Identification and separation analysis of wave components of the wind sea and swell provide a more realistic depiction of the sea state and is important for understanding of the mechanisms of climate variability in the wave field. Spectral separating is one of the most important methods in partitioning waves. Two separating methods including the initial wave steepness method (STPN) and modified wave steepness method (MSTPN) that proposed by the National Data Buoy Center (NDBC) are described in this paper. And the NDBC buoy observations are applied in this study to investigate STPN and MSTPN. Although MSTPN method is improved from the STPN method, it is still not fit for the swell effect. Considering limitations mentioned above, we use spectral energy proportion (SEP) to describe the swell effect and abstract the valid data according to this index. Finally, we give a description of correlation between significant wave height (SWH) and wind speed under the wind sea condition. From results, it is shown that SWH and wind speed of wind sea have a quasi-quadratic fitting relationship. In addition, it shows that MSTPN is a better performance in application as expected. Our work for spectral partitioning algorithms could provide a reference for the future work in satellite spectral data. And a practical method for deriving the SWHs from wind speed of scatterometer will be realized on the basis of the empirical wind and sea relationship.
机译:由局部风力场产生的遥远来源和风水膨胀的共存导致复杂的表面波条件。风海波波部件的识别和分离分析,膨胀提供了对海水位的更现实的描述,对波田气候变异机制的理解是重要的。光谱分离是分隔波中最重要的方法之一。本文介绍了国家数据浮标中心(NDBC)提出的初始波陡度法(STPN)和改性波陡法(MSTPN)的两个分离方法。在本研究中应用NDBC浮标观察以调查STPN和MSTPN。尽管从STPN方法改进了MSTPN方法,但它仍然不适合膨胀效果。考虑到上述限制,我们使用光谱能量比例(SEP)来描述膨胀效果并摘要根据该指数的有效数据。最后,我们在风海条件下提供了显着波浪高度(SWH)和风速之间的相关性的描述。从结果中,显示风海的SWH和风速具有准二次拟合关系。此外,它表明,MSTPN在应用程序中是更好的性能。我们对光谱分区算法的工作可以为卫星谱数据的未来工作提供参考。并在经验风和海关系的基础上实现从散射仪风速衍生SWH的实用方法。

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