摘要：This paper presents a two-basin model of the water and heat balances of the Western and Eastern Mediterranean sub-basins (WMB and EMB, respectively) over the 1958-2010 period using available meteorological and hydrological data. The results indicate that the simulated temperature and salinity in both studied Mediterranean sub-basins closely follow the reanalysed data. In addition, simulated surface water in the EMB had a higher mean temperature (by approximately 1.6^oC) and was more saline (by approximately 0.87gkg^-^1) than in the WMB over the studied period. The net evaporation over the EMB (1.52mmday^-^1) was approximately 1.7 times greater than over the WMB (0.88mmday^-^1). The water balance of the Mediterranean Sea was controlled by net inflow through the Gibraltar Strait and Sicily Channel, the net evaporation rate and freshwater input. The heat balance simulations indicated that the heat loss from the water body was nearly balanced by the solar radiation to the water body, resulting in a net export (import) of approximately 13 (11)Wm^-^2 of heat from the WMB (to the EMB).
