Abstract
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.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
