黄海苏北滩慢阻波及其近几十年的气候变化

X. Liang
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引用次数: 0

摘要

海岸捕获波(CTWs)是天气频带中的一类亚惯性信号,在沿海海气相互作用中起着关键作用。然而,这个重要的话题似乎在最近几年关于沿海环境变化和保护的激烈辩论中被忽视了。在本章,abriefbutself-containedintroductionoftheCTWtheoryispresented inthehopeofprovidingareferenceforinvestigatorsintherelevantfields。给出了计算波浪特性的数值格式。为了证明这一点,我们已经对黄海苏北岸的河段进行了初步的研究。因此,自20年前以来,所有计算出的慢模态,包括底部强化模态,似乎都在下降。当强厄尔尼诺现象Niño为followedbyastrongLaNiña时,比如97 - 98和09 - 10ElNiñoevents,它们的速度会特别慢。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The Slow Coastal-Trapped Waves off Subei Bank in the Yellow Sea and Their Climatic Change in the Past Decades
Coastal-trappedwaves (CTWs) areaclassofsubinertial signalsin theweatherfrequencyband that playa pivotal role in coastal air-sea interaction. However, this important topic seems to be missingintheheateddebateinrecentyearsoncoastalenvironmentalchangeandprotection.In thischapter,abriefbutself-containedintroductionoftheCTWtheoryispresented,inthehopeofprovidingareferenceforinvestigatorsintherelevantfields.Alsopresentedisanumerical scheme for computing the wave properties. As a demonstration, we have conducted a prelim-inarystudyoftheCTWsforasectionacrosstheSubeiBankintheYellowSea.Bytheresults,allthecomputedslowmodes,includingabottom-intensifiedone,seemtobeslowingdownsince two decades ago. They have particularly slowed down in the event when a strong El Niño is followedbyastrongLaNiña,suchasinthe97 – 98and09 – 10ElNiñoevents.
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