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- W2205003721 abstract "The Aegean Sea is an eastern Mediterranean sub-basin with highly complex bathymetry, high seasonal variations in temperature, considerable fresh water fluxes, and large gradients in salinity or temperature across neighbouring water masses (Black Sea and Eastern Mediterranean). To simulate the hydrography of the Aegean Sea, a primitive equation, time-dependent, free surface, split mode time-step model (hereafter the Aegean model) has been developed that solves the continuity and momentum equations, the conservation equations for heat and salinity, and makes use of the turbulence closure scheme of Mellor and Yamada [10]. In the work reported herein, the Aegean model is coupled with an advection-diffusion model to study the dense water formation processes in the North Aegean Sea (N. Aegean Trough), where the most dense waters of Mediterranean have been observed. The model uses as external forcing historical wind stress data, precipitation data. Thermal fluxes at the sea surface boundary are computed interactively from wind, air temperature and relative humidity. The water mass flowing from the Black Sea through the Bosporus and the Dardanelles to the Aegean Sea is also introduced using measured seasonal vertical profiles of temperature and salinity." @default.
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- W2205003721 date "1970-01-01" @default.
- W2205003721 modified "2023-09-23" @default.
- W2205003721 title "Investigation Of The Deep Water Formation InThe N. Aegean Sea Basin" @default.
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- W2205003721 doi "https://doi.org/10.2495/hy940132" @default.
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