派博傳思國(guó)際中心

標(biāo)題: Titlebook: Extreme Ocean Waves; Efim Pelinovsky,Christian Kharif Book 2016Latest edition Springer International Publishing Switzerland 2016 Extreme O [打印本頁(yè)]

作者: 迅速    時(shí)間: 2025-3-21 17:21
書目名稱Extreme Ocean Waves影響因子(影響力)




書目名稱Extreme Ocean Waves影響因子(影響力)學(xué)科排名




書目名稱Extreme Ocean Waves網(wǎng)絡(luò)公開(kāi)度




書目名稱Extreme Ocean Waves網(wǎng)絡(luò)公開(kāi)度學(xué)科排名




書目名稱Extreme Ocean Waves被引頻次




書目名稱Extreme Ocean Waves被引頻次學(xué)科排名




書目名稱Extreme Ocean Waves年度引用




書目名稱Extreme Ocean Waves年度引用學(xué)科排名




書目名稱Extreme Ocean Waves讀者反饋




書目名稱Extreme Ocean Waves讀者反饋學(xué)科排名





作者: 出汗    時(shí)間: 2025-3-21 23:01
An Analytical Model of Large Amplitude Internal Solitary Waves, 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: eardrum    時(shí)間: 2025-3-22 01:58
https://doi.org/10.1007/978-3-319-21575-4Extreme Ocean Waves; Freak Waves; Hydrodynamic Model; Mechanisms of Ocean Waves; Physics of Wave Formati
作者: 實(shí)施生效    時(shí)間: 2025-3-22 05:41
https://doi.org/10.1007/978-94-6300-968-3We compare applicability of the recently derived compact equation for surface wave with the fully nonlinear equations. Strongly nonlinear phenomena, namely modulational instability and breathers with the steepness . are compared in numerical simulations using both models.
作者: 比賽用背帶    時(shí)間: 2025-3-22 09:42

作者: 河流    時(shí)間: 2025-3-22 14:32

作者: 河流    時(shí)間: 2025-3-22 19:11

作者: 睨視    時(shí)間: 2025-3-23 00:50
978-3-319-33095-2Springer International Publishing Switzerland 2016
作者: 的事物    時(shí)間: 2025-3-23 03:05

作者: Concomitant    時(shí)間: 2025-3-23 07:53
Klaus Beutel,Hans-Peter Fischer for strong departures from Gaussian-and second-order-based statistics. For finite water depth, on the contrary, wave instability attenuates and eventually vanishes for relative water depths as low as . (where . is the wavenumber of the dominant waves and . the water depth). Experimental results, no
作者: 咽下    時(shí)間: 2025-3-23 11:30

作者: Pastry    時(shí)間: 2025-3-23 17:31
https://doi.org/10.1007/978-3-658-09171-2l 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: 蛙鳴聲    時(shí)間: 2025-3-23 19:05

作者: ARIA    時(shí)間: 2025-3-24 00:28

作者: 蟄伏    時(shí)間: 2025-3-24 04:16

作者: N斯巴達(dá)人    時(shí)間: 2025-3-24 09:28

作者: 表狀態(tài)    時(shí)間: 2025-3-24 11:05
https://doi.org/10.1007/978-3-031-12922-3able cliff into the sea can generate a tsunami wave near the coast and exhibit extreme run-up. As a result, those tsunamis develop significant hazards to the population. The threat caused by such tsunamis strongly depends on the topography and location of the unstable cliff. Predicting the height of
作者: 小蟲    時(shí)間: 2025-3-24 17:15

作者: Accommodation    時(shí)間: 2025-3-24 22:04
https://doi.org/10.1007/978-3-319-03656-4 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: 創(chuàng)作    時(shí)間: 2025-3-25 02:22
Occurrence of Extreme Waves in Finite Water Depth,ics and particularly on the occurrence of extremes. Despite evidence of modulational instability in regular wave fields, results presented herein seems to indicates that wave instability has a negligible effect on wave statistics, which remains primarily affected by second-order contributions.
作者: Incise    時(shí)間: 2025-3-25 04:26
Searching for Factors that Limit Observed Extreme Maximum Wave Height Distributions in the North Seumental response in measuring maximum wave height. The data indicate that steepness is a limiting factor for extreme wave height. At the shallow water location, extreme waves are not more frequently observed than at the deep water location. The relation between the freak wave index of the ECMWF wave
作者: 不朽中國(guó)    時(shí)間: 2025-3-25 10:58
Extremes and Decadal Variations in the Baltic Sea Wave Conditions,m in cyclone Gudrun in January 2005. No clear trend exists in the wave properties in the Baltic Sea. The 99?%-iles of the significant wave height exhibit a complicated spatial pattern of changes and have significantly decreased between the islands of ?land and Gotland and to the south of these islan
作者: Middle-Ear    時(shí)間: 2025-3-25 13:16

作者: originality    時(shí)間: 2025-3-25 17:06

作者: Bravura    時(shí)間: 2025-3-25 23:52

作者: accrete    時(shí)間: 2025-3-26 03:27
https://doi.org/10.1007/978-3-322-83434-8m in cyclone Gudrun in January 2005. No clear trend exists in the wave properties in the Baltic Sea. The 99?%-iles of the significant wave height exhibit a complicated spatial pattern of changes and have significantly decreased between the islands of ?land and Gotland and to the south of these islan
作者: BAN    時(shí)間: 2025-3-26 06:43
Book 2016Latest editionave theories. In addition, recent results on tsunami waves due to subaerial landslides are presented. This book is written for specialists in the fields of fluid mechanics, applied mathematics, nonlinear physics, physical oceanography and geophysics, and for students learning these subjects.
作者: arabesque    時(shí)間: 2025-3-26 09:02
Thermal Diffusion in a Polymer Blend,ion 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: 樹(shù)木心    時(shí)間: 2025-3-26 16:19

作者: chalice    時(shí)間: 2025-3-26 19:04
https://doi.org/10.1007/978-3-031-12922-3f the tsunami waves. We also present triphasic numerical simulations based on a finite-volume method where different rheologies are considered for the slide. We also emphasize the difficulty of such simulations and compare the numerical results to experimental measurements.
作者: 阻撓    時(shí)間: 2025-3-26 21:37
,Rogue Waves in Higher Order Nonlinear Schr?dinger Models,ion 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: 五行打油詩(shī)    時(shí)間: 2025-3-27 01:44

作者: 圣歌    時(shí)間: 2025-3-27 07:10

作者: resuscitation    時(shí)間: 2025-3-27 11:44

作者: Consequence    時(shí)間: 2025-3-27 17:12

作者: 脖子    時(shí)間: 2025-3-27 21:16
Modeling of Rogue Wave Shapes in Shallow Water, The variable-polarity shape of a rogue wave is more probable than only one crest or one trough, because the generation of the latter ones needs a specific phase relation between individual waves in the group.
作者: legacy    時(shí)間: 2025-3-27 23:53

作者: 土產(chǎn)    時(shí)間: 2025-3-28 03:56
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 the average runup height of waves with wide spectrum is higher than of waves with narrow spectrum.
作者: 吵鬧    時(shí)間: 2025-3-28 09:35
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 three-wave resonant system. Implementation in Mathematica is given for planetary ocean waves. Short discussion concludes the paper.
作者: 散布    時(shí)間: 2025-3-28 11:04

作者: 切碎    時(shí)間: 2025-3-28 17:51

作者: 山頂可休息    時(shí)間: 2025-3-28 21:50

作者: 翅膀拍動(dòng)    時(shí)間: 2025-3-29 00:48

作者: EXPEL    時(shí)間: 2025-3-29 03:35

作者: 向下五度才偏    時(shí)間: 2025-3-29 08:12
Occurrence of Extreme Waves in Finite Water Depth, for strong departures from Gaussian-and second-order-based statistics. For finite water depth, on the contrary, wave instability attenuates and eventually vanishes for relative water depths as low as . (where . is the wavenumber of the dominant waves and . the water depth). Experimental results, no
作者: 巡回    時(shí)間: 2025-3-29 13:57

作者: Annotate    時(shí)間: 2025-3-29 17:02
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: 懶鬼才會(huì)衰弱    時(shí)間: 2025-3-29 23:42

作者: Presbyopia    時(shí)間: 2025-3-30 03:44

作者: 圖表證明    時(shí)間: 2025-3-30 06:37

作者: 聲音刺耳    時(shí)間: 2025-3-30 11:34

作者: Nonthreatening    時(shí)間: 2025-3-30 15:02
Tsunami Waves Generated by Cliff Collapse: Comparison Between Experiments and Triphasic Simulationsable cliff into the sea can generate a tsunami wave near the coast and exhibit extreme run-up. As a result, those tsunamis develop significant hazards to the population. The threat caused by such tsunamis strongly depends on the topography and location of the unstable cliff. Predicting the height of




歡迎光臨 派博傳思國(guó)際中心 (http://www.pjsxioz.cn/) Powered by Discuz! X3.5
苏尼特左旗| 邢台县| 东乡| 布尔津县| 延寿县| 南通市| 原阳县| 会东县| 开原市| 河间市| 内江市| 加查县| 荥经县| 三门县| 抚宁县| 德江县| 长子县| 大悟县| 锦屏县| 苗栗县| 二手房| 昌乐县| 玉田县| 桂东县| 星子县| 红河县| 六枝特区| 新民市| 青河县| 马山县| 介休市| 黑龙江省| 贵德县| 平凉市| 顺义区| 临安市| 广水市| 遂川县| 泽州县| 云南省| 台中县|