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Extraction of spatial-temporal rules from mesoscale eddies in the South China Sea based on rough set theory

机译:基于粗糙集理论的南海中尺度涡旋时空规律提取

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摘要

In this paper, a rough set theory is introduced to represent spatial-temporal relationships and extract the corresponding rules from typical mesoscale-eddy states in the South China Sea (SCS). Three decision attributes are adopted in this study, which make the approach flexible in retrieving spatial-temporal rules with different features. The results demonstrate that this approach is effective, and therefore provides a powerful approach to forecasts in the future studies. Spatial-temporal rules in the SCS indicate that warm eddies following the rules are generally in the southeastern and central SCS around 2000m isobaths in winter. Their intensity and vorticity are weaker than those of cold eddies. They usually move a shorter distance. By contrast, cold eddies are in 2000m and deeper regions of the southwestern and northeastern SCS in spring and fall. Their intensity and vorticity are strong. Usually they move a long distance. In winter, a few rules are followed by cold eddies in the northern tip of the basin and southwest of Taiwan Island rather than warm eddies, indicating cold eddies may be well-regulated in the region. Several warm-eddy rules are achieved west of Luzon Island, indicating warm eddies may be well-regulated in the region as well. Otherwise, warm and cold eddies are distributed not only in the jet flow off southern Vietnam induced by intraseasonal wind stress in summer-fall, but also in the northern shallow water, which should be a focus of a future study.
机译:本文引入了一种粗糙集理论来表示时空关系,并从南海典型的中尺度涡旋状态中提取相应的规则。本研究采用了三个决策属性,这使得该方法可以灵活地检索具有不同特征的时空规则。结果表明该方法是有效的,因此为将来的研究提供了强有力的预测方法。 SCS中的时空规则表明,遵循该规则的暖涡通常发生在冬季2000m等深处的东南和中部SCS。它们的强度和涡度比冷涡旋的弱。他们通常移动较短的距离。相比之下,冷涡在春季和秋季分别位于2000m和西南和东北南海的更深区域。它们的强度和涡度很强。通常他们会移动很远的距离。在冬季,在盆地北端和台湾岛西南部遵循一些规则的冷涡,而不是暖涡,这表明该地区的冷涡可能受到良好的调节。在吕宋岛以西达成了几条暖涡规则,这表明暖涡在该地区也可能受到良好的监管。否则,温暖和寒冷的涡流不仅会分布在夏季秋季的季节内风应力引起的越南南部喷射流中,而且会分布在北部浅水区,这将是未来研究的重点。

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