scholarly journals A physical model for the narrowing of the directional sea wave spectra in the short gravity to gravity-capillary range

2002 ◽  
Vol 107 (C10) ◽  
Author(s):  
Gérard Caudal
Keyword(s):  
2008 ◽  
Vol 237 (21) ◽  
pp. 2767-2776 ◽  
Author(s):  
A.O. Korotkevich
Keyword(s):  

2016 ◽  
Vol 52 (9) ◽  
pp. 888-903 ◽  
Author(s):  
V. G. Bondur ◽  
V. A. Dulov ◽  
A. B. Murynin ◽  
Yu. Yu. Yurovsky

Author(s):  
Hermione J. van Zutphen ◽  
Philip Jonathan ◽  
Kevin C. Ewans

We report a new approach to model the frequency-direction spectrum, in which the frequency-direction spectra from measurements or hindcast studies are fitted simultaneously in two dimensions, frequency and direction. Depending on the amount of wind forcing on the partition, either a unimodal (swell) or bimodal (wind-sea) wave spreading function is adopted together with the spectral form which best fits the frequency spectrum. This paper describes the new method and presents the results on a measured dataset.


SIMULATION ◽  
2019 ◽  
Vol 96 (3) ◽  
pp. 281-296
Author(s):  
Sekil Park ◽  
Jinah Park

The sea has a very wide, irregular, and continuously changing surface and is usually a mixed sea composed of several wave systems. Each wave system is generated from different locations and conditions and has its own characteristics. The Fourier domain approach using sea wave spectra is an effective technique for the realistic simulation of sea surfaces in real time, but the conventional Fourier domain approach cannot independently simulate the characteristics of each wave system. In this paper, we propose a realistic and real-time simulation method of the mixed sea using multiple spectrum-based wave systems for maritime simulators. We recognize the importance of the visual and physical contributions of each wave system and faithfully reproduce all wave systems in the mixed sea. In order to simulate the mixed sea, our method generates and combines multiple spectrum-based wave systems using adaptive spectral sampling of the separated spectrum of the multi-peaked spectrum. The unique characteristics of each wave system can be set independently through spectral parameters, sampling number and range, wave direction and spread, and the shape factor of waves. The proposed method also supports the smooth transition between sea states, such as wind sea, swell, and mixed sea. Through the experiments, we verify that the proposed method effectively reflects sea wave spectra and the reproduced sea has very similar statistical characteristics to the actual sea. Experimental results also show that our approach can simulate the mixed sea, which has high-frequency wind sea and low-frequency swell.


Author(s):  
Victor I. Titov ◽  
Victor Bakhanov ◽  
A. A. Demakova ◽  
Irina A. Sergievskaya ◽  
Aleksey Kuzmin ◽  
...  
Keyword(s):  

2016 ◽  
Vol 52 (6) ◽  
pp. 637-648 ◽  
Author(s):  
V. G. Bondur ◽  
V. A. Dulov ◽  
A. B. Murynin ◽  
V. Yu. Ignatiev

1980 ◽  
Vol 1 (17) ◽  
pp. 20 ◽  
Author(s):  
P.E. Dexter ◽  
R.C. Casey

The possibility of deriving parameters of sea wave spectra remotely from characteristics of radio waves at high frequency (HF) scattered from the sea surface was first raised when Crombie (1955) correctly deduced that Doppler frequency shifts in the signal returned from short range in his HF radar resulted uniquely from components of the sea wave spectrum having wavelengths exactly one-half the radio wavelength, and travelling radially with respect to the radar. Since then the technique has been expanded in two directions: (a) The use of ionospherically propagated-JiF radio waves ('Skywave' HF radar) to^ examine extensive ocean areas out to some 4000 km from the observing site, to obtain oceanographic and meteorological data suitable for input to synoptic observation systems. This approach has been developed through the experimental work of Tveten (1967) and Ward (1969), and the empirical technique proposed by Long and Trizna (1973) to allow the simple extraction of sea surface wind vectors from Doppler spectra of the backscattered radio signals. (b) The determination of directional sea wave spectra and sea surface currents at short ranges with HF radars operating in the groundwave propagation mode, based on theoretical analyses of the scattering process such as those of Barrick (1972). The HF Skywave radar constructed and operated at Townsville by the Physics Department of James Cook University has been employed for some years now on research into the possibilities for mapping sea states and sea surface winds over ocean areas surrounding Australia (Ward, 1969; Ward and Dexter, 1976; Dexter and Casey, 1978).


1984 ◽  
Vol 11 (2) ◽  
pp. 185-207 ◽  
Author(s):  
C. Guedes Soares
Keyword(s):  

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