Qianru Niu, Yanqing Feng, Si Chen, Yan Li, Jianghua Lv, Hanxiang Su, Lin Mu
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引用次数: 0
Abstract
Using 30-year simulations (1990–2020) with a validated third-generation wave model, we investigated how El Niño-Southern Oscillation (ENSO) drives seasonal wave climate variability in the northern South China Sea (SCS). Results reveal distinct ENSO impacts across seasons. Spring/winter waves respond to monsoon shifts, with El Niño reducing wave heights and La Niña amplifying extreme waves (the 95th-percentile significant wave heights, Hs95) via intensified winter monsoon. An exception occurs in the Gulf of Tonkin, where El Niño elevates Hs95 during the winter monsoon season through localized resonance. Summer/fall waves vary with ENSO's reorganization of tropical cyclone (TC) tracks aligning with ENSO-modulated subtropical ridge changes. Specifically, Eastern Pacific (EP) El Niño concentrates TC near the Luzon Strait, boosting extreme waves in the northeast SCS. Fall coastal energy declines under EP El Niño corresponding to the suppressed basin-wide TC activity. The findings advance predictive insights for the wave climate in monsoon and TC-driven subtropical marginal seas under ENSO variability, addressing the need for localized climate adaptation strategies in marginal seas that are under multi-scale atmospheric forcing.
利用30年(1990-2020)的第三代波浪模式模拟,研究了El Niño-Southern涛动(ENSO)驱动南海北部季节波浪气候变率的机制。结果显示不同季节ENSO的影响不同。春冬波响应季风变化,El Niño降低浪高,La Niña通过增强的冬季季风放大极端波(第95百分位显著波高,Hs95)。东京湾是个例外,在冬季季风季节,El Niño通过局部共振使Hs95升高。夏季/秋季波随ENSO重组的热带气旋(TC)路径与ENSO调制的副热带高压脊变化对齐而变化。具体而言,东太平洋(EP) El Niño将TC集中在吕宋海峡附近,促进了南海东北部的极端海浪。EP El Niño下海岸能量下降,对应于全盆地TC活动的抑制。这些发现为ENSO变率下季风和tc驱动的亚热带边缘海波浪气候提供了预测见解,解决了在多尺度大气强迫下边缘海局部气候适应策略的需求。