1995
DOI: 10.1175/1520-0485(1995)025<2853:tsoniw>2.0.co;2
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The Structure of Near-Inertial Waves during Ocean Storms

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Cited by 47 publications
(55 citation statements)
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“…The 100-m lower core could be explained by the appearance of a second wave group from west of the moorings, as investigated by Qi et al (1995). This is not ruled out in our observations.…”
Section: Internal Wave Activitymentioning
confidence: 56%
See 1 more Smart Citation
“…The 100-m lower core could be explained by the appearance of a second wave group from west of the moorings, as investigated by Qi et al (1995). This is not ruled out in our observations.…”
Section: Internal Wave Activitymentioning
confidence: 56%
“…The Ocean Storms Experiment (see Oceans Storms collection of papers: D 'Asaro 1995a,b,c;Niiler and Paduan 1995;Large and Crawford 1995;Qi et al 1995;Zervakis and Levine 1995;Levine and Zervakis 1995;Large et al 1995) was an effort to examine more closely the processes of air-sea interaction using a collection of moored and drifting instruments, and our interest here is the response of the mixed layer to surface forcing and the mechanisms responsible for the momentum transfer below the mixed layer. We approach this through analysis of previously unreported moored observations taken during Ocean Storms for two distinct autumn storms with clear but dramatically different upper-ocean responses.…”
Section: Introductionmentioning
confidence: 99%
“…4c and 5c). According to the method utilized in Qi et al (1995), the downward group velocity (c gz ) can be estimated via the ratio of the vertical migration of the near-inertial groups and the corresponding time period (Fig. 5c).…”
Section: Summary Of the Observed Internal Wavesmentioning
confidence: 99%
“…Besides, the correlation between the near-inertial waves and strong surface forcing is lagged in time. It is found that the gradual propagation of storm induced inertial waves into the thermocline that lasted many days after the initiation of the storm based on the Ocean Storm Experiment in the northeast Pacific Ocean (Qi et al 1995). Three cycles of a single, energetic, downward-propagating near-inertial wave associated with enhanced mixing were observed in the Banda Sea (Alford and Gregg 2001).…”
Section: Introductionmentioning
confidence: 99%
“…In order to estimate quantitatively the downward energy propagation of these events we computed the correlation coefficient of the complex near‐inertial velocity, D , within the time interval [10–40] days, with a reference depth at the upper level z 1 = 240 m. This coefficient is computed using the following expression [see also Qi et al , 1995, equation (8)]: …”
Section: Focus On Events Of High‐amplitude Inertia‐gravity Wavesmentioning
confidence: 99%