標題: Titlebook: Dynamics of Ocean Tides; G. I. Marchuk,B. A. Kagan Book 1989 Kluwer Academic Publishers 1989 Tide.energy.formation.ocean.satellite [打印本頁] 作者: BROOD 時間: 2025-3-21 17:44
書目名稱Dynamics of Ocean Tides影響因子(影響力)
書目名稱Dynamics of Ocean Tides影響因子(影響力)學(xué)科排名
書目名稱Dynamics of Ocean Tides網(wǎng)絡(luò)公開度
書目名稱Dynamics of Ocean Tides網(wǎng)絡(luò)公開度學(xué)科排名
書目名稱Dynamics of Ocean Tides被引頻次
書目名稱Dynamics of Ocean Tides被引頻次學(xué)科排名
書目名稱Dynamics of Ocean Tides年度引用
書目名稱Dynamics of Ocean Tides年度引用學(xué)科排名
書目名稱Dynamics of Ocean Tides讀者反饋
書目名稱Dynamics of Ocean Tides讀者反饋學(xué)科排名
作者: 草率男 時間: 2025-3-21 22:36
Bruno Chaudet,Valérie Carayol,Alex Frame equilibrium tide in the ocean, presented in section 1.4, indicate that the opposite is true. But ocean tides are not in equilibrium, and the question, there fore, remains open. Provinding the answer to this question is the object of this chapter.作者: 戰(zhàn)役 時間: 2025-3-22 03:28
Toni Muzi Falconi,Fabio Ventoruzzont boundary layer remains hydrodynamically stable up to the moment when its effective Reynolds number.If we now define the thickness of the turbulent boundary layer as δ. = (2v./σ). we obtain the estimate . where . . is the tidal velocity amplitude outside the boundary layer; σ is the oscillation frequency.作者: Overdose 時間: 2025-3-22 07:12 作者: STENT 時間: 2025-3-22 12:02
Betteke van Ruler,Anne-Marie Cottoneasurements containing the values of harmonic tidal constants at 108 stations located in different parts of the World Ocean, and accumulated up to 1977, have been systematized by Cartwright et. al. [104].作者: 惰性女人 時間: 2025-3-22 15:30
Lars?ke Larsson,Tor Bang,Finn Frandsenompressible, and long (including tidal) waves are selected out of the family of gravitational oscillations, proceeding from the requirement of the smallness of the ratio between the vertical and the horizontal scales of motion. From the continuity equation it then follows that vertical velocities are small in comparison with the horizontal ones.作者: 惰性女人 時間: 2025-3-22 20:22 作者: BRIEF 時間: 2025-3-22 21:36 作者: antenna 時間: 2025-3-23 04:36 作者: 遺留之物 時間: 2025-3-23 08:41 作者: 一個攪動不安 時間: 2025-3-23 13:33 作者: deriver 時間: 2025-3-23 15:13 作者: semble 時間: 2025-3-23 21:08
https://doi.org/10.1007/978-94-009-2571-7Tide; energy; formation; ocean; satellite作者: 監(jiān)禁 時間: 2025-3-24 00:42 作者: caldron 時間: 2025-3-24 05:38 作者: Intuitive 時間: 2025-3-24 06:34 作者: Lethargic 時間: 2025-3-24 12:23 作者: Fatten 時間: 2025-3-24 14:51 作者: Connotation 時間: 2025-3-24 20:27 作者: Sad570 時間: 2025-3-25 01:51 作者: accordance 時間: 2025-3-25 03:37
Betteke van Ruler,Anne-Marie Cotton or automatic level recorders. The accuracy of such measurements in approximately 1 cm. At present there exist some ten thousand stations, scores of them having accumulated continuous series of hourly elevation measurements of more than 50 years duration. Since 1964 deep-sea recording instruments wi作者: 悅耳 時間: 2025-3-25 09:59
Lars?ke Larsson,Tor Bang,Finn Frandsenforced oscillations generated by the major harmonics of the tidal potential. That is why the general hydrodynamic equations having solutions corresponding to all the components of the spectrum should be modified in much a way as not to contain any extraneous solutions and, at the same time, not to d作者: 打折 時間: 2025-3-25 11:49 作者: 殘暴 時間: 2025-3-25 18:41 作者: 小木槌 時間: 2025-3-25 23:07
Toni Muzi Falconi,Fabio Ventoruzzonge rapidly from zero to its value in the external flow, corresponding to the flow of an ideal fluid (fluid without viscosity). The lower part of the where noticeable changes in the velocity are taking place, caused by the influence of the ocean bottom, is known as ..作者: Oratory 時間: 2025-3-26 00:07 作者: jaundiced 時間: 2025-3-26 08:23
Oceanographic Sciences Libraryhttp://image.papertrans.cn/e/image/284145.jpg作者: 休戰(zhàn) 時間: 2025-3-26 08:34
Methods and Results of Experimental Studies of Ocean Tides, or automatic level recorders. The accuracy of such measurements in approximately 1 cm. At present there exist some ten thousand stations, scores of them having accumulated continuous series of hourly elevation measurements of more than 50 years duration. Since 1964 deep-sea recording instruments wi作者: d-limonene 時間: 2025-3-26 13:58
Qualitatives Studies of the Tidal Dynamics Equations,forced oscillations generated by the major harmonics of the tidal potential. That is why the general hydrodynamic equations having solutions corresponding to all the components of the spectrum should be modified in much a way as not to contain any extraneous solutions and, at the same time, not to d作者: 暖昧關(guān)系 時間: 2025-3-26 20:05 作者: AVID 時間: 2025-3-26 21:07 作者: fallible 時間: 2025-3-27 01:11 作者: 有常識 時間: 2025-3-27 06:52
Bottom Boundary Layer in Tidal Flow: Theoritical Models,e we introduce the effective coefficient of vertical turbulent viscosity ., constant with height, and, following Charney [72], assume that the turbulent boundary layer remains hydrodynamically stable up to the moment when its effective Reynolds number.If we now define the thickness of the turbulent 作者: 調(diào)色板 時間: 2025-3-27 13:18 作者: Synovial-Fluid 時間: 2025-3-27 14:14
Tides in the Ocean-Shelf System,itions on what is going on in the open sea.” One of the possible reasons for the failure of the theoretical approach to describing quantitatively the tides in the open sea is associated with disregard for shelf effects.作者: FIN 時間: 2025-3-27 19:20
8樓作者: 小臼 時間: 2025-3-27 22:39
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9樓作者: commensurate 時間: 2025-3-28 16:56
9樓作者: Incommensurate 時間: 2025-3-28 21:31
10樓作者: 愚蠢人 時間: 2025-3-29 00:10
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