Abstract
A diurnal cycle in temperature and vertical displacement variance has been observed in the stratified region below the surface mixed layer using moored time-series data at 0°, 140°W for three periods: November 1984, April 1987, and May-June 1987. The amplitude of the cycle during each of the experiments, and the likely causes of variance are discussed. -after Authors
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CITATION STYLE
McPhaden, M. J., & Peters, H. (1992). Diurnal cycle of internal wave variability in the equatorial Pacific Ocean: results from moored observations. Journal of Physical Oceanography, 22(11), 1317–1329. https://doi.org/10.1175/1520-0485(1992)022<1317:DCOIWV>2.0.CO;2
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