作者: Outspoken 時(shí)間: 2025-3-21 22:38
Non-Gaussian Properties of Shallow Water Waves in Crossing Seas,ing wave trains generates steep and high amplitude peaks, thus enhancing the deviation of the surface elevation from the Gaussian statistics. The analysis of the skewness and the kurtosis shows that the statistical properties depend on the angle between the two wave trains.作者: Acquired 時(shí)間: 2025-3-22 04:14
Runup of Long Irregular Waves on Plane Beach,represents an irregular sea state with Gaussian spectrum. The asymptotic of probability functions in the range of large amplitudes for estimation of freak wave formation in the shore is studied. It is shown that average runup height of waves with wide spectrum is higher than that of waves with narrow spectrum.作者: 門閂 時(shí)間: 2025-3-22 08:00
Symbolic Computation for Nonlinear Wave Resonances,efined by (1) integer solutions of the resonance conditions, and (2) coupling coefficients of the dynamical system on the wave amplitudes. General computation algorithms are presented which can be used for arbitrary 3-wave resonant system. Implementation in Mathematica is given for planetary ocean waves. Short discussion concludes the paper.作者: Melatonin 時(shí)間: 2025-3-22 10:21 作者: 大約冬季 時(shí)間: 2025-3-22 16:22 作者: 大約冬季 時(shí)間: 2025-3-22 20:37 作者: Choreography 時(shí)間: 2025-3-22 22:36
https://doi.org/10.1007/978-3-540-77831-8represents an irregular sea state with Gaussian spectrum. The asymptotic of probability functions in the range of large amplitudes for estimation of freak wave formation in the shore is studied. It is shown that average runup height of waves with wide spectrum is higher than that of waves with narrow spectrum.作者: FECT 時(shí)間: 2025-3-23 03:02
Fuyin Wei,Cyril Alias,Bernd Nocheefined by (1) integer solutions of the resonance conditions, and (2) coupling coefficients of the dynamical system on the wave amplitudes. General computation algorithms are presented which can be used for arbitrary 3-wave resonant system. Implementation in Mathematica is given for planetary ocean waves. Short discussion concludes the paper.作者: periodontitis 時(shí)間: 2025-3-23 09:15 作者: aptitude 時(shí)間: 2025-3-23 12:44 作者: 豐滿有漂亮 時(shí)間: 2025-3-23 15:28 作者: Dealing 時(shí)間: 2025-3-23 21:19
https://doi.org/10.1007/978-3-322-90543-7ion and increased likelihood of rogue waves; (b) the extreme waves intermittently emerging from the chaotic background can be correlated with the homoclinic orbits characterized by maximal coalescence of their spatial modes.作者: Glucocorticoids 時(shí)間: 2025-3-23 23:18
Ondrej Ja?ko,Ivan Todorovi?,Stefan KomazecExtreme wave conditions with .. ≥ 7m have been registered five times since 1978. The records overlook 2–3 such cases. The overall recorded maximum .. is 7.8 m. The estimated maximum of .. was 9.5 m in cyclone Gudrun in January 2005.作者: jealousy 時(shí)間: 2025-3-24 03:20 作者: 憤怒歷史 時(shí)間: 2025-3-24 07:41 作者: Genome 時(shí)間: 2025-3-24 12:35 作者: Compass 時(shí)間: 2025-3-24 18:18 作者: inferno 時(shí)間: 2025-3-24 20:57
Book 20081st editionn instability of nonlinear wave field, physical and statistical properties of rogue wave generation in deep water and in shallow water, various models of nonlinear water waves, special analysis of nonlinear resonances between water waves and the relation between observations and freak wave theories.作者: 敲詐 時(shí)間: 2025-3-25 03:07 作者: ELUDE 時(shí)間: 2025-3-25 06:40
Freak Waves: Peculiarities of Numerical Simulations,f the fluid to the lower half-plane. We have considered two problems: (i) modulation instability of wave train and (ii) evolution of nonlinear Shr?dinger equation solitons with different steepness of carrier wave. In both cases we have observed formation of freak waves.作者: Intact 時(shí)間: 2025-3-25 08:47
,Rogue Waves in Higher Order Nonlinear Schr?dinger Models,ion and some of its higher order generalizations. Numerical investigations and analytical arguments based on the inverse spectral theory of the underlying integrable model, perturbation analysis, and statistical methods provide a coherent picture of rogue waves associated with nonlinear focusing eve作者: 開始從未 時(shí)間: 2025-3-25 15:40
Non-Gaussian Properties of Shallow Water Waves in Crossing Seas,l properties of random shallow water waves in constant depth for crossing sea states. Numerical simulations indicate that the interaction of two crossing wave trains generates steep and high amplitude peaks, thus enhancing the deviation of the surface elevation from the Gaussian statistics. The anal作者: 提名的名單 時(shí)間: 2025-3-25 19:31 作者: 現(xiàn)代 時(shí)間: 2025-3-25 22:14 作者: GRUEL 時(shí)間: 2025-3-26 00:46
Symbolic Computation for Nonlinear Wave Resonances, one of the possible processes yielding the appearance of independent wave clusters which keep their energy. Energetic behavior of these clusters is defined by (1) integer solutions of the resonance conditions, and (2) coupling coefficients of the dynamical system on the wave amplitudes. General com作者: custody 時(shí)間: 2025-3-26 08:20
Searching for Factors that Limit Observed Extreme Maximum Wave Height Distributions in the North Sehether steepness and shallow water effects are limiting factors for extreme wave heights. The relation between observations and a model freak wave index is examined..Measurements from two locations in the North Sea are used, one with a depth of 80 m, and another with a depth of 20 m. The data consis作者: 國家明智 時(shí)間: 2025-3-26 11:28 作者: Horizon 時(shí)間: 2025-3-26 13:09
Extreme Waves Generated by Cyclones in Guadeloupe,tructive and murderous. The extreme waves caused by cyclones on the coast of Guadeloupe for a whole historic period are discussed. The first documented sea damage during hurricane passage in Guadeloupe occurred in 1642. Data of extreme waves induced by hurricanes from 1928 to 2007 in Guadeloupe are 作者: 脖子 時(shí)間: 2025-3-26 17:40 作者: 寬度 時(shí)間: 2025-3-27 01:02 作者: BOLT 時(shí)間: 2025-3-27 01:13
http://image.papertrans.cn/f/image/320038.jpg作者: 奴才 時(shí)間: 2025-3-27 05:49
https://doi.org/10.1007/978-1-4020-8314-3Ocean; Oceanography; fluid mechanics; geophysics; nonlinear physics; physical oceanography; rogue waves作者: OPINE 時(shí)間: 2025-3-27 13:30 作者: goodwill 時(shí)間: 2025-3-27 14:27 作者: Resistance 時(shí)間: 2025-3-27 21:19 作者: mastoid-bone 時(shí)間: 2025-3-28 00:54
Lehre als interdisziplin?re Herausforderung A particular attention is paid to the formation of troughs in front of high crests. The conditions for appearance of the ‘three sisters’ are discussed too. It is important to emphasize that this mechanism is not too sensitive to the variation of the shape of transient frequency modulated wave group作者: 不整齊 時(shí)間: 2025-3-28 04:57 作者: 匍匐前進(jìn) 時(shí)間: 2025-3-28 07:18 作者: covert 時(shí)間: 2025-3-28 14:19
Manfred Hessenberger,Hans-Christian Krcalhether steepness and shallow water effects are limiting factors for extreme wave heights. The relation between observations and a model freak wave index is examined..Measurements from two locations in the North Sea are used, one with a depth of 80 m, and another with a depth of 20 m. The data consis作者: 無瑕疵 時(shí)間: 2025-3-28 18:19
Ondrej Ja?ko,Ivan Todorovi?,Stefan Komazecong-term time series from Almagrundet (1978–2003) and Vilsandi (1954–2005), and wave statistics from the middle of the northern Baltic Proper. The typical wave periods are 3–4 s in coastal areas and 4–6 s on the open sea. The monthly mean wave height varies from about 0.4 (0.5) m in April–July to 0.作者: AGGER 時(shí)間: 2025-3-28 20:48 作者: parsimony 時(shí)間: 2025-3-28 23:27
Jennie G. Noll,Margalit Roitman the lower layer and with exponentially stratified fluid in the upper layer. The long-wave approximation is constructed by means of implementing a scaling procedure with a small Boussinesq parameter. Extreme configurations of solitary waves such as broad table-top waves are discussed.作者: intention 時(shí)間: 2025-3-29 06:50
978-90-481-7839-1Springer Science+Business Media B.V. 2008作者: Contend 時(shí)間: 2025-3-29 09:15
Horst Meier,Christoph S. Zollerf the fluid to the lower half-plane. We have considered two problems: (i) modulation instability of wave train and (ii) evolution of nonlinear Shr?dinger equation solitons with different steepness of carrier wave. In both cases we have observed formation of freak waves.
