期刊
JOURNAL OF PHYSICAL OCEANOGRAPHY
卷 37, 期 4, 页码 1066-1076出版社
AMER METEOROLOGICAL SOC
DOI: 10.1175/JPO3032.1
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A 50-day time series of high-resolution temperature in the deepest layers of the Canada Basin in the Arctic Ocean indicates that the deep Canada Basin is a dynamically active environment, not the quiet, stable basin often assumed. Vertical motions at the near-inertial (tidal) frequency have amplitudes of 10-20 m. These vertical displacements are surprisingly large considering the downward near-inertial internal wave energy flux typically observed in the Canada Basin. In addition to motion in the internal-wave frequency band, the measurements indicate distinctive subinertial temperature fluctuations, possibly due to intrusions of new water masses.
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