Research Article

Model Thermohaline Trends in the Mediterranean Sea during the Last Years: A Change with Respect to the Last Decades?

Table 1

Linear trends of temperature ( 𝑇 , °C/year), salinity ( 𝑆 , year−1) and steric sea level ( 𝜉 𝑆 , cm/year) for the Mediterranean Sea from ECCO (E), and GLORYS (G) models. The time periods spanned are also indicated.

𝑆 E ( 9 3 - 0 9 ) 1 0 3 𝑆 E ( 0 2 - 0 9 ) 1 0 3 𝑆 G ( 0 2 - 0 9 ) 1 0 3 𝑇 E ( 9 3 - 0 9 ) 1 0 3 𝑇 E ( 0 2 - 0 9 ) 1 0 3 𝑇 G ( 0 2 - 0 9 ) 1 0 3 𝜉 S E ( 9 3 - 0 9 ) 𝜉 S E ( 0 2 - 0 9 ) 𝜉 S G ( 0 2 - 0 9 )

0–150 1 . 4 ± 0 . 1 1 . 3 ± 0 . 4 6 ± 3 5 ± 3 1 2 ± 1 2 ( 1 ) 1 5 ± 1 2    ( 1 ) n.s.n.s.n.s.
150–600 2 . 4 4 ± 0 . 0 6 0 . 6 8 ± 0 . 0 9 4 . 1 ± 0 . 2 n.s. 1 7 ± 2 1 7 ± 2 0 . 1 0 0 ± 0 . 0 0 3 0 . 1 6 ± 0 . 0 7 0 . 3 0 ± 0 . 0 2
600-bottom 1 . 0 7 ± 0 . 0 2 1 . 1 8 ± 0 . 0 5 9 ± 1 8 . 0 0 ± 0 . 0 9 7 . 7 ± 0 . 2 9 . 3 ± 0 . 2 0 . 3 2 1 ± 0 . 0 0 2 0 . 3 4 6 ± 0 . 0 0 6 0 . 6 7 ± 0 . 0 2
0-bottom 1 . 7 7 ± 0 . 0 7 0 . 9 ± 0 . 1 1 0 ± 1 n.s.n.s. ( 2 ) n.s.   ( 2 ) 0 . 2 8 ± 0 . 0 1 0 . 3 2 ± 0 . 0 4 1 . 0 1 ± 0 . 0 6

( 1 ) Although the trend for the entire period 02–09 is subject to large uncertainty, two intervals of different trend can be identified: from 02 to 06, a negative trend of − 0 . 1 0 ± 0 . 0 2 °C/year and − 0 . 1 2 ± 0 . 0 2 °C/year for ECCO and GLORYS, respectively, is observed, followed by a positive trend of 0 . 1 6 ± 0 . 0 3 °C/year (ECCO) and 0 . 1 5 ± 0 . 0 4 °C/year (GLORYS) in 06–09.
( 2 ) The same as above is applicable for the entire water column with negative trends of − 0 . 0 3 9 ± 0 . 0 0 7 °C/year (ECCO) and − 0 . 0 5 ± 0 . 0 1 °C/year (GLORYS) in 02–06 that change to positive 0 . 0 5 ± 0 . 0 1 °C/year (the same for both models) in 06–09.