“…There is a rich diversity of models available to conduct climate change projections in coastal areas, such as GETM, FESOM-C, SCHISM/SELFE, NEMO, DELFT3D, ROMS, FVCOM, and others (Burchard and Bolding, 2002;Shchepetkin and McWilliams, 2005;Chen et al, 2006;Zhang and Baptista, 2008;Zhang et al, 2016;Madec et al, 2017;Androsov et al, 2019). The role of the physical models can be divided into four pieces: (1) predictions of the abiotic parameters' distribution in space and time to supply the biogeochemical and food-web models (Hofmeister et al, 2017;Kerimoglu et al, 2017;Lemmen et al, 2018), (2) prediction of pathways of water parcels, passive and active tracers (van der Molen et al, 2018;Ricker and Stanev, 2020;Sprong et al, 2020), (3) predictions of the future "hotspots" in a sense of largest changes in the abiotic parameters' behavior (sensitivity studies) (Delworth et al, 2012;Yin, 2012;Schrum et al, 2016), and (4) evaluation of the representativeness of long-term observational stations for larger areas.…”