摘 要: | In El Nino years, along the southeast China coast, the seasonal cycle of sea level variation - low in spring, high in autumn - is attenuated: specifically, the autumn peak is reduced by about 10 cm. This negative anomaly increases toward the south and occurs at the same time as a similar (but five times larger) sea level anomaly at Truk Island (7.5°N) in the western Pacific.
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