Abstract
The interannual variability of the Kuroshio volume transport passing through the 137°E meridian south of Japan was simulated with an ocean general circulation model (OGCM). The time series of the Kuroshio volume transport over the 1000 m depth in the OGCM is well reproduced by the one-dimensional quasi-geostrophic (QG) vorticity equation with a windstress forcing. In our analysis of the OGCM and QG results, we found that peaks and troughs of the time series of the Kuroshio volume transport with 2–3 yr time-scale were induced by windstress curl, both local and immediately eastward, whereas longer time-scale variability was also induced by windstress curl near the dateline.
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Wakata, Y., Setou, T., Kaneko, I. et al. Interannual variability of the Kuroshio transport passing through the 137°E meridian in an OGCM related to the North Pacific windstress. J Oceanogr 62, 25–35 (2006). https://doi.org/10.1007/s10872-006-0029-7
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DOI: https://doi.org/10.1007/s10872-006-0029-7