The three dimensional model with the affection of stratified density (Caspian Sea)


Autoria(s): Hadjimobini, Susan
Data(s)

2005

Resumo

The hydro dynamical actions in big Lakes directly influence dynamic, physical and chemical affairs. The circulation's models and temperature have something to do with the movements of fluids, and analysis for circulation in Caspian sea is because of the lack of observation through which the circulations and out comings are determined. Through the studies, three dimensional simulations (Large- Scale) are planned and performed, according to Smolakiewicz and Margolin works. This is a non- hydrostatic and Boussinesq approximation is used in its formulation is used in its formulation on the basis of Lipps (1990) theorem and curve lines, the fluid is constant adiabatic and stratified, and the wind power is considered zero. The profile of speed according to previous depth and before ridge can be drawn on the basis of density available between northern and southern ridges. The circulation field is drawn from 3 cm/s to 13 cm/s on the plate z= 5 cm , the vertical changes of speed on the plate is 0.02 m/s. Vertical profile , horizontal speed in previous on, and after the ridges on are drawn on different spaces. It changes from 0.5 cm/s to 1 cm/s before ridges.

Formato

application/pdf

Identificador

http://aquaticcommons.org/20565/1/11533.pdf

Hadjimobini, Susan (2005) The three dimensional model with the affection of stratified density (Caspian Sea). PhD Thesis, Islamic Azad University, Science and Research Branch, Tehran, 115pp.

Idioma(s)

fa

Relação

http://aquaticcommons.org/20565/

Palavras-Chave #Engineering #Oceanography
Tipo

Thesis

NonPeerReviewed