Caspian Sea Water Surface Oscillations and Dynamics of Dust and Sandstorms

The Caspian Sea, as the largest enclosed inland body of water globally, undergoes notable fluctuations in its water levels controlled by various factors such as atmospheric conditions, river inflow, and regional climate patterns. Studies, including the CASHKI model, have demonstrated the significant role of the Caspian Sea in the dynamics of dust and sandstorms, particularly in Central Asia and Eastern Iran. This research aims to precisely understand the interconnected dynamics and explore the intricate relationship between Caspian Sea water surface oscillations and the dynamic patterns of dust and sandstorms in surrounding regions. Using a comprehensive approach involving satellite data analysis, numerical simulations, and statistical modeling, the study identifies discernible patterns and trends in Caspian Sea water surface oscillations. It sheds light on the potential correlation between these oscillations and the occurrence, intensity, and propagation of dust and sandstorms. Furthermore, the research investigates the atmospheric and climatic conditions that may either amplify or mitigate the impact of these water surface oscillations on the generation and propagation of dust and sandstorms The findings of this study contribute to a better understanding of the complex interactions between large water bodies and atmospheric phenomena, emphasizing the potential role of Caspian Sea dynamics in influencing regional dust and sandstorm dynamics. Such insights are crucial for developing effective strategies to mitigate these natural events' environmental and societal impacts on the affected areas.