Abstract
Twenty-two years (1967-88) of hydrographic data collected along the 137°E meridian and surface wind data were analyzed. In the midlatitude region north of 22°N, the dominant signal in the dynamic height field was the interannual path variations of the Kuroshio. In the low-latitude region along 137°E, fluctuations in the surface height anomaly field had a meridionally coherent structure, and large surface height drops coincided with the ENSO events in the tropical Pacific. -from Authors
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CITATION STYLE
Bo Qiu, & Joyce, T. M. (1992). Interannual variability in the mid- and low-latitude western North Pacific. Journal of Physical Oceanography, 22(9), 1062–1079. https://doi.org/10.1175/1520-0485(1992)022<1062:ivitma>2.0.co;2
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