Author: Leif N. Thomas
Publisher:
ISBN:
Category : Ocean-atmosphere interaction
Languages : en
Pages : 134

View

Book Description

Author: Henk A. Dijkstra
Publisher: Springer Science & Business Media
ISBN: 140202262X
Category : Science
Languages : en
Pages : 548

View

Book Description
Taken from a review of the first edition in SIAM: "This text is different from most others in that it combines several different disciplines and draws on many scientific studies in order to deduce mechanisms of ocean circulation. (...) Therefore (it) cannot be substituted, and (...) it meets its unique goals with clarity and thoroughness".

Author: Vitalii A. Sheremet
Publisher:
ISBN:
Category : Ocean circulation
Languages : en
Pages : 452

View

Book Description

Author: Gerhard Neumann
Publisher:
ISBN:
Category : Ocean currents
Languages : en
Pages : 40

View

Book Description

Author: Gerhard Neumann
Publisher:
ISBN:
Category : Ocean-atmosphere interaction
Languages : en
Pages : 72

View

Book Description

Author: Allan R. Robinson
Publisher:
ISBN:
Category : Ocean circulation
Languages : en
Pages : 184

View

Book Description

Author: Worth D. Nowlin
Publisher:
ISBN:
Category : Ocean circulation
Languages : en
Pages : 198

View

Book Description
Considered are steady, wind-driven currents in a two-layer model ocean, confined within a rectangular basin with a horizontal sea bed. The horizontal velocities are assumed independent of elevation within each layer of this finite difference approximation to the continuously stratified real ocean. Neglecting nonlinear field accelerations, a frictional model for the entire basin is formulated which allows for vertical, but not horizontal, transfer of horizontal momentum due to turbulence. The exchange of horizontal momentum between layers and to the sea bed is provided through the assumption of interlayer and bottom stresses, which are assumed proportional to the vertical contrast of horizontal velocity across the appropriate interface. The constants of proportionality, which are estimated from considerations of the observed circulation, play decisive roles in controlling the circulation patterns within each layer and the internal dissipation of energy from the steady organized flow. The solution, obtained for a purely zonal wind stress which varies latitudinally as a cosine, depicts an anticyclonic circulation within the lower layer which is intensified more to the west than is the anticyclonic gyre within the upper layer. Numerical calculations were performed for a range of physical parameters. ...

Author: Andrew Elek Kiss
Publisher:
ISBN:
Category : Ocean circulation
Languages : en
Pages : 152

View

Book Description

Author: Sybren S. Drijfhout
Publisher: Elsevier Inc. Chapters
ISBN: 0128058609
Category : Science
Languages : en
Pages : 68

View

Book Description
Conceptual models are a vital tool for understanding the processes that maintain the global ocean circulation, both in nature and in complex numerical ocean models. In this chapter we provide a broad overview of our conceptual understanding of the wind-driven circulation, the thermohaline circulation, and their transient behavior. While our conceptual understanding of the time-mean wind-driven circulation is now fairly mature, basic questions remain regarding the thermohaline circulation, for example, surrounding its overall strength and stability. Similarly, basic questions remain regarding the transient adjustment and internal variability of the ocean circulation.

Author: Julian P. McCreary
Publisher:
ISBN:
Category : Ocean circulation
Languages : en
Pages : 76

View

Book Description