Presentation of the first terrarium effect model of sea water and ocean salinity in analogy to the reflection of geophysical periodic balance with the closed climate relativity hypothesis

Articles in Press

Author

Department of Resource Management, Faculty of Management, Islamic Azad University, Independent Comprehensive Branch, Najaf Abad City, Isfahan, Iran

Abstract

The salinity of sea and ocean water is an important geophysical parameter in the study of climate change and a fundamental factor in understanding the dynamics of the seas. The purpose of the model is to present the trend of water salinity. According to the aforementioned model, the pressure due to the air around the Earth in the closed enclosure of the atmosphere, which is simulated by the walls of the terrarium, acts as a regulator of periodic volumetric balance or semi-permeable curtain. In the long term, the terrarium model states that salinity determines the volumetric scale of the equilibrium dynamic pressure through the reflection of the comparative balance in terms of weight and volume in the classification of similarity. The model seeks to explore the outcome of three factors: 1. Water 2. Land 3. Air pressure: including the volume of the climatic air of the region, in the comparison of the dynamics of the exchange of relativity. The result of a graph with a dynamic approach is the positive incremental fluctuation of this relativity. Each of the above factors is a dependent variable, and changes in external factors such as temperature, pressure, the rate of melting of the Earth's glaciers, etc. can disrupt the balance between these three factors. The salinity of the water will gradually increase and will reach a stability reflecting the periodic volume balance of geophysics. Again, by changing one of the dependent variables, the subset undergoes positive sinusoidal changes.

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Articles in Press, Accepted Manuscript
Available Online from 01 July 2025

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