Published In
Geophysical Research Letters
Document Type
Article
Publication Date
2-1-2009
Subjects
Sea level -- Climatic factors -- Pacific Ocean, Tides -- Pacific Ocean -- Environmental impact analysis
Abstract
Global sea level (GSL) rise is well documented. However, changes in high waters, including the tidal contribution, are sometimes more relevant than GSL rise. Analysis of 34 long tidal records from the Eastern Pacific Ocean shows that K1 and M2 amplitudes (∣K₁∣ and ∣M₂∣) are increasing, except for ∣M2∣ in the Gulf of Panama. North of 18°N, ∣K1∣ and ∣M2∣ are both growing at 2.2% century⁻¹. The mean increase in total tidal amplitude (0.59 mmyr⁻¹) is less than the present GSL rise (1.7 mmyr⁻¹). However, mean sea level is nearly constant in the NE Pacific, so tidal evolution plays a major regional role in changes in high water levels. The spatial pattern of tidal evolution suggests the influence of large-scale processes, and the similarity in spatial patterns for ∣K₁∣ and ∣M₂∣ excludes mechanisms with strong frequency dependence. Increasing tidal amplitudes may impact ocean mixing, nutrient supply, primary production, fisheries, and coastal erosion.
DOI
10.1029/2008GL036185
Persistent Identifier
http://archives.pdx.edu/ds/psu/7991
Citation Details
Jay, D. A. (2009), Evolution of tidal amplitudes in the eastern Pacific Ocean, Geophys. Res. Lett., 36, L04603
Description
This is the publisher's final PDF. Copyright 2009 American Geophysical Union.