What is it about?
The interannual sea-level variability in the Philippine Sea is mainly driven by ENSO. It takes three months for sea level to respond to temperature anomalies in the Niño 3.4 region. Temperature increase (decrease) in the Niño 3.4 region results in the northward (southward) shift of the NBL after two months. The northward (southward) shift in NBL then results in decrease (increase) in sea level after a month, and sea level also increases or decreases in phase with SST.
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Why is it important?
This study is important because El Niño Southern Oscillation (ENSO) highly influence the climate and oceanographic dynamics of the Philippines
Read the Original
This page is a summary of: Influence of the El Niño Southern Oscillation to the interannual sea-level variability in the Philippine Sea, January 2023, Elsevier,
DOI: 10.1016/b978-0-323-91708-7.00003-1.
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