29 °C) using the RCP26 scenario check details to 2.53 °C (1.63 °C) using the RCP85 scenario (data not shown). In general, there is significant variability in seasonal warming, expressed as SST, during the current century for the different CMIP5 ensemble mean scenarios. The Mediterranean

Sea SST is projected to warm significantly in each scenario, especially in summer (2.92–0.47 °C century− 1), as seen in Figure 7b. Similarly, the AAM sub-basin is projected to warm significantly, ranging from a maximum of 1.68–0.31 °C century− 1 in summer to a minimum of 1.35–0.29 °C century− 1 in winter. Moreover, the Black Sea is also projected to warm significantly, ranging from a maximum of 2.81–0.53 °C century− 1 in summer to a minimum of 2.33–0.51 °C century− 1 in winter (data not shown). click here Mediterranean Sea surface variability

is affected by a combination of oceanic and atmospheric processes and displays significant regional and seasonal behaviour. AVHRR gridded annual SST data over the Mediterranean Sea indicate a range of 3.5 °C between a maximum SST of 21.2 °C over the Levantine sub-basin and a minimum SST of 17.7 °C over the LPC sub-basin. These data also indicate a seasonal SST range of 10 °C, ranging from 15.2 °C in winter, through 18.8 °C in spring and 19.8 °C in autumn, to 25 °C in summer. The Mediterranean SST is significantly warming by 0.35 °C decade− 1, with a seasonal trend variability peaking in spring at 0.38 °C decade− 1 followed by 0.32 °C decade− 1 in summer, 0.22 °C decade− 1 in autumn and 0.160 °C decade− 1 in winter. However, the Black Sea (AAM sub-basin) displays a higher (lower) warming trend of 0.51 °C decade− 1 (0.24 °C decade− 1). This Tau-protein kinase annual Mediterranean warming trend agrees with the previous findings of Nykjaer (2009) and Skliris et al. (2012) but runs counter to those of D’Ortenzio et al. (2000). The disagreement with D’Ortenzio et al. (2000) is probably due to the examination of different time periods. However, the annual Black Sea SST warming trend found here is less significant than the trends calculated by Belkin (2009), probably because

Belkin’s study period extends only to 2002. The spatial distribution of SST warming trends leads to significant eddies distributed over the Mediterranean Sea, indicating significant changes in the Mediterranean Sea surface circulation in the near future. The SST warming trends in the various Mediterranean sub-basins are more (less) significant than the SST warming trends in the AAM sub-basin (Black Sea). Similarly, the COV values for the SSTs of the various Mediterranean sub-basins are higher (lower) than those for the AAM sub-basin (Black Sea). At the 95% significance level, the monthly Mediterranean SST is significantly affected by atmospheric temperature (R = 98%), total cloud cover (R = − 0.81), solar radiation to the open water surface (R = 72%), net heat loss from the sea (R = − 53%), precipitation (R = − 0.53), SLP (R = − 0.43), eastward wind stress (R = − 0.