Designing a Numerical Model to Study the Effect of Tide and Wind in a Theoretical Basin in Similarity to Persian Gulf

Zamanian, Mohammad Taghi; Sadrinasab, Masoud; Fallahi, Mehri

doi:10.22113/jmst.2019.149922.2203

Document Type : Original Manuscript

Authors

¹ Atmospheric Science and Meteorological Research Center, Iran Meteorological Organization, Tehran, Iran.

² Department of environment, Technical Faculties Campus (Environment), University of Tehran, Tehran, Iran.

³ Department of Marine Physics, Factually of Marine Science and Oceanography, Khorramshahr University of Marine Science and Technology, Khorramshahr, Iran.

https://doi.org/10.22113/jmst.2019.149922.2203

Abstract

The design of oceanic numerical model for Persian Gulf to predict oceanic phenomena and parameters is one of the most important ways of preventing or solving problems environment and designing of the oceanic model similar to it is an effective method that can explain physical response of environment to different situations. Purpose of this research is designing oceanic numerical model for environment similar to Persian Gulf, to predict its reaction in return effect of tide and wind. This three-dimensional model based on primitive equations in spherical coordinates system with sigma vertical coordinate. To solve equations of model is used finite difference method. Compared with similar models, model framework and calculate more logical tension between are the benefits of this model. An oceanic five-layer basin is considered with maximum and minimum depth 100m and 80.09m. The average daily wind in Persian Gulf, the average daily salinity and water temperature and the changes in the water level in Strait of Hormuz are used in this model. The two-year implementation of model showed that in this basin, the tidal force is a dominant force compared with windy force and density gradient, also the maximum current in strait is 1.98 m/s which can create anticlockwise circulation in basin. Maximum total change of water height is 2.98 m in relation to the static level. Implementation results of this model correspond to the oceanographic reality of Persian Gulf, while matches with purpose; it is the basis of suitable model for Persian Gulf.

Keywords

20.1001.1.20088965.1401.21.1.3.0

Main Subjects

فیزیک دریا

References

Anderson Jr. John D. 1995. Computational fluid dynamics the basics with applications. McGraw-Hill, Inc, p547

Aple J.R. 1990. Principles of ocean physics. London Academic Press, p 634

Brewer P.G., Fleer A. P., Kadar S., Shafer D. L. and Smith C. L. 1978. Chemical Oceanography Data from the Persian Gulf and Gulf of Oman. Woods Hole Oceanography Institution Technical Report. 78-37, 105 pp.

Farjami H., Zamanian M.T. and Azarm Sa S.A. 2006. Numerical Simulation of Wind Induced Current in Artificial Five-Layer Ocean Basin. MSc Thesis. Department of physical oceanography, Faculty of Natural Resources and Marine Sciences, Tarbiat modares University, Tehran, Iran. 108p.

Farjami H., Zamanian M., Rashidi Ebrahim Hesari A. and Azarmsa, S.A. 2012. Numerical Simulation of Ekman Theory in Five Layers Oceanic Basin. Journal of Marine Science and Technology, 11(1): 41-48.

Haltiner G.J. and Williams R.T. 1980. Numerical prediction and dynamic meteorology. John Wiley and sons, Pp. 250

Heidari Nesheli Z., Zamanian M.T. and Sadrinasab M. 2018. Desigen of Oceanic Model for Caspian Sea. PhD Thesis, Faculty of Marine Science, Khorramshahr University of Marine Science and Technology, Iran, 194p.

Heidari Nesheli Z., Zamanian M.T. and Sadrinasab M. 2018. Wind Effect on Changes of Density in a Theoretical Oceanic Model with Non-Level Bottom. Hydrophysics, 2(2): 27-40.

Ibrayev R. A., Zsoy E. O., Schrum S. and Sur H. (2010). Seasonal variability of the Caspian Sea three dimensional circulation sea level and air-sea interaction. Ocean Science Discuss, Vol. 6, p. 1913-1970.

Kantha L. and Clayson C. 2000. Numerical models of oceans and oceanic processes. San Diego, Academic Press, pp: 1-490.

Nihoul J. C. 1977. Three-dimensional model of tides and storm surges in a shallow well-mixed continental sea. Dynamics of Atmospheres and Oceans, 2(1), 29–47

Reynolds R. M., 1993. Physical oceanography of the Gulf, Strait of Hormuz and the Gulf of Oman Results from the Mt Mitchell expedition. Mar. Pollution Bull., 27, 35–59.

Rashidi Ebrahim Hesari A., Zamanian M. T. and Azarmsa, S.A. 2006. Simulation of Tidal Current in Two Layers Oceanic Basin by Three Dimensional Numerical Model. Journal of Marine Science and Technology, 4(3-4): 13-22.

Kämpf J. 2009. Advanced Ocean Modelling. Flinders University, School of the Environment, PO Box 2100 Adelaide SA 5001, Australia, 193p

Thorp S. A. 2009. Wind stress coefficients over sea surface from breeze to hurricane. Journal of Geophysics Res., 78: 9704-9706.

Wright J. L., 1974. A hydrographic and acoustic survey of the Persian Gulf, MSc Thesis, Nav. Postgrad. Sch., Monterey, Calif.

Zamanian M. T. 2006. Project of base model two layered. Institute of Meteorology and Atmospheric Science.

Zamanian M. T. 1994. Three Dimensional Models for Persian Gulf. PhD Thesis. University of the Philippines, 162p.

Designing a Numerical Model to Study the Effect of Tide and Wind in a Theoretical Basin in Similarity to Persian Gulf

References

References

Volume 21, Issue 1March 2022Pages 27-38

Volume 21, Issue 1
March 2022
Pages 27-38