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

AVID

fallible

有常識

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

調(diào)色板

Synovial-Fluid

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.

FIN

8樓

小臼

8樓

CRATE

9樓

Left-Atrium

9樓

Ergots

9樓