Titlebook: Dynamics of Ocean Tides; G. I. Marchuk,B. A. Kagan Book 1989 Kluwer Academic Publishers 1989 Tide.energy.formation.ocean.satellite

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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

草率男

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.

戰(zhàn)役

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.

Overdose

STENT

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].

惰性女人

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.

惰性女人

BRIEF

antenna

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