Abstract
Sea-level measurements along the western coast of the Americas have shown that there is a strong signal at ENSO frequencies that propagates poleward at about 40 to 90 cm s-1. A near-boundary numerical model with realistic bottom friction, stratification, and shelf and slope topography was constructed to study ENSO coastal flow. -from Authors
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CITATION STYLE
APA
Clarke, A. J., & Van Gorder, S. (1994). On ENSO coastal currents and sea levels. Journal of Physical Oceanography, 24(3), 661–680. https://doi.org/10.1175/1520-0485(1994)024<0661:OECCAS>2.0.CO;2
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