Observations made with an array of wave sensors reveal significant differences between the high-frequency regions of spectra measured on different days. These differences suggest that the idea of a universal equilibrium range may not be strictly true
A sequence of ten records of the directional wave spectrum has been obtained from the motions of a f...
From the Global Weather Experiment in 1979, four one-year data records are juxtaposed which simultan...
The proper ties of free unattenuated long waves of small amplitude that travel parallel to the coast...
This paper is concerned with the dynamical processes involved in the growth of the lower frequency s...
A section of sea surface that had been subjected to a constant offshore wind was profiled by using a...
Correlations between laboratory and geophysical data are presented for certain statistical propertie...
Autospectra of observed particle motions in ocean waves are presented. The spectra show the dominant...
Water-surface slopes due to wind waves have been measured in a laboratory windwave tunnel. In all me...
The atmospheric pressure field above waves was monitored at two experimental sites in the Bight of A...
This paper describes a series of field experiments that provide growth curves and wind histories for...
Mapping of wave trains during four flights over the ocean off southern California showed the consist...
A study is conducted into the response of sea level and dynamic height to fluctuations of alongshore...
As part of the POLYMODE experiment, three clusters (labeled A, B, C) of moored current meters and te...
Hydrographic data at Ocean Station Echo (35N, 48W) form an almost continuous 6-year series ending in...
Sea-surface temperature and atmospheric pressure records during the past 40 years indicate that an i...
A sequence of ten records of the directional wave spectrum has been obtained from the motions of a f...
From the Global Weather Experiment in 1979, four one-year data records are juxtaposed which simultan...
The proper ties of free unattenuated long waves of small amplitude that travel parallel to the coast...
This paper is concerned with the dynamical processes involved in the growth of the lower frequency s...
A section of sea surface that had been subjected to a constant offshore wind was profiled by using a...
Correlations between laboratory and geophysical data are presented for certain statistical propertie...
Autospectra of observed particle motions in ocean waves are presented. The spectra show the dominant...
Water-surface slopes due to wind waves have been measured in a laboratory windwave tunnel. In all me...
The atmospheric pressure field above waves was monitored at two experimental sites in the Bight of A...
This paper describes a series of field experiments that provide growth curves and wind histories for...
Mapping of wave trains during four flights over the ocean off southern California showed the consist...
A study is conducted into the response of sea level and dynamic height to fluctuations of alongshore...
As part of the POLYMODE experiment, three clusters (labeled A, B, C) of moored current meters and te...
Hydrographic data at Ocean Station Echo (35N, 48W) form an almost continuous 6-year series ending in...
Sea-surface temperature and atmospheric pressure records during the past 40 years indicate that an i...
A sequence of ten records of the directional wave spectrum has been obtained from the motions of a f...
From the Global Weather Experiment in 1979, four one-year data records are juxtaposed which simultan...
The proper ties of free unattenuated long waves of small amplitude that travel parallel to the coast...