Abstract
Always oceanographers pay attention to layer structure in the sea environment. Creation of layer structures is because of some phenomenons like double diffusion, internal waves, turbulence modular mixing. In this paper with examination of vertical structure of temperature, salinity and density between Persian Gulf and Oman Sea in different seasons, layer structures appear clearly. Also, countors of the same physical parameters show the existence of regular structure which prove internal waves resulting from the Persian Gulf and flow into the Oman Sea.
Highlights
Always oceanographers pay attention to layer structures in the sea environment
When salinity and temperature distribution in water column has a upside down effects with regard to density distribution, very interesting structures can be created in water column which is called double diffusion convection
The occurrence of double diffusion convection is due to three basic factors permanently and naturally in most of oceans and seas: According to studies and given numerical models, the input flow of fresh water via Strait of Hormoz due to decreasing the north western winds power, increasing buoyancy forces, increasing south western monsoon and stratification in Oman Sea, reaches the end of the Persian Gulf
Summary
The Physical Study of Vertical Structure of Temperature, Salinity and Density Layer Structure Between Persian Gulf and Oman Sea. Abdoreza Sabet Ahd, Hesameddin Mehrfar2* and Mina Mohammadi Pasand3 1Collage of Basic Science, jahrom Branch, Iran 2Department of Physics, University of Ayatollah Ozma Borujerdi, Borujerd, Iran 3Department of Marine Physics, Institute of Geophysics University of Tehran, Tehran, Iran *Corresponding author: Hesameddin Mehrfar, Department of Physics, University of Ayatollah Ozma Borujerdi, Borujerd, Iran
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