Kilometer-scale trends and variability of the Adriatic present climate (1987–2017)

• Published in: Climate dynamics 2023-09, Vol.61 (5-6), p.2521-2545
• Main Authors: Tojčić, Iva, Denamiel, Cléa, Vilibić, Ivica
• Format: Article
• Language: English
• Subjects: Advection; Analysis; Atmosphere; Atmospheric models; Climate change; Climate models; Climatic changes; Climatology; Deep water; Earth and Environmental Science; Earth Sciences; Environmental aspects; Geophysics/Geodesy; In situ measurement; Inflow; Influence; Intermediate water; Intermediate water masses; Modelling; Ocean models; Ocean-atmosphere interaction; Oceanography; Oceans; Outflow; Regional climate models; Regional climates; Relative humidity; Remote sensing; Salinity; Seasonal variability; Temperature; Temperature trends; Thermohaline circulation; Trends; Variability; Water circulation; Wind speed
• ISSN: 0930-7575; 1432-0894
• DOI: 10.1007/s00382-023-06700-2

We present the Adriatic atmosphere–ocean trends and variability simulated by the kilometer-scale Adriatic Sea and Coast (AdriSC) climate model during the 1987–2017 period. As the AdriSC model has been successfully validated over the entire basin against an extensive dataset of in situ measurements and remote sensing products, the reliability of the presented results at the regional (basin-wide) and local (sub-domains) scales is high. We found that trends and variability in the atmosphere reveal strong land-sea contrasts with (1) stronger temperature trends associated with lower, mostly seasonal, variability over the Adriatic Sea than over the land and (2) positive trends of wind speed and negative trends of relative humidity associated with high, mostly seasonal, variability over the sea and vice versa over the land. While, in the ocean, the analysis highlights several processes: (1) extensive warming by the atmosphere at the surface during summer, affecting both temperature and salinity, (2) shallowing of the advection of the saline Levantine Intermediate Water inflow into the Adriatic, (3) decrease of the Adriatic deep water outflow and therefore the Adriatic-Ionian thermohaline circulation, (4) warming of near-bottom waters, in particular in the middle and northern Adriatic, and (5) shrinking and weakening of the Southern Adriatic Gyre, in particular at its center. We thus demonstrate that kilometer-scale coupled atmosphere–ocean modelling is an indispensable tool for proper quantification of climate change in complex coastal basins, as it captures local characteristics not properly reproduced by present state-of-the-art regional climate models with an order of magnitude coarser resolutions.