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High-Frequency Components of Ocean Waves and Their Relation to the Aerodynamic Roughness
High-Frequency Components Aerodynamic Roughness Ocean Waves
2009/4/2
Ocean waves of high frequency (from about 10 to 200 rad sec−1) were observed by means of a thin capacitance-type wave gage. The representative rms height, hp, of the sea-surface irregularities a...
Measurement of the High-Frequency Spectrum of Ocean Surface Waves
High-Frequency Spectrum Ocean Surface Waves
2009/3/7
High-frequency spectra of wind-generated ocean waves were measured at an ocean research tower of Kyushu University using a fast-response wave recorder and an electronic differentiating circuit. Wind w...
Observed Interaction between Low and High Frequency Motions off the Coasts of Peru and California
High Frequency low frequency Peru California
2008/12/27
Datasets taken near the coasts of Peru and California have been analyzed to explore the evidence of a correlation between the high frequency (period < 10.8 hour) and low frequency (period > 4 day) mot...
The Influence of Horizontal Inhomogeneities on the Propagation of High-Frequency Linear Internal Gravity Waves across a Baroclinic Flow
Horizontal Inhomogeneities Baroclinic Flow Linear Internal Gravity Waves
2008/12/22
The effect of the inclusion of the horizontal gradients of background density and baroclinic flow on the propagation of linear internal gravity wave packets across the flow is investigated using ray-t...
High-Frequency Internal Waves at 0°, 140°W and Their Possible Relationship to Deep-Cycle Turbulence
surface mixed layer High-Frequency Internal Waves Deep-Cycle Turbulence
2008/12/9
An analysis of a moored time series at 0°, 140°W from November to December 1991 found a nighttime enhancement of isotherm displacement variance and of zonal velocity variance below the surface mixed l...
Forcing and Sampling of Ocean General Circulation Models：Impact of High-Frequency Motions
Ocean General Circulation Models High-Frequency Motions
2008/11/18
Significant inertial oscillations are present in all primitive equation ocean general circulation models when they are forced with high-frequency (period order of days) wind stress fields. At specific...
