Coherence of internal tide modulations along the Hawaiian Ridge

Long time series of sea level from tide gauges along the north side of the Hawaiian Ridge and shorter series of dynamic heights inferred from inverted echo sounders moored just north of the main Hawaiian Islands are examined for evidence of internal tides at the M-2 frequency. We find that the ampli tudes and phases of the M-2 tidal components have low-frequency variability , which is consistent with a superposition of an internal tide with the lar ger barotropic tide. Further, the low-frequency variability is correlated w ith low-frequency changes in the depth of the pycnocline, which suggests a simple physical mechanism to account for the low-frequency modulations in t he internal tidal amplitude. These modulations are coherent for long distan ces along the Hawaiian Ridge, indicating a coherent generation of the inter nal tide that is consistent with acoustic observations in the North Pacific and with recent analyses of sea surface heights from satellite altimetry.