Stepped Coastal Water Warming Revealed by Multiparametric Monitoring at NW Mediterranean Fixed Stations.

In a coastal area of the NW Mediterranean, an increasing trend of 0.014 °C yr −1 has been reported from 1974 to 2006 [ 8 ].

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The turbidity anomaly in the whole water column (i.e., 2–200 m depth) showed a trend to decrease from about 0.03 FTU in 2010 to −0.07 FTU in 2017 (~0.1 FTU), with the inshore station presenting the highest variability in 2013 ( Figure 8 , Figure S3 ).

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