“…Besides, an increasing body of empirical studies are applying the results of mesocosm experiments conducted in tidal creeks designed to test the effects of elevation relative to sea level (i.e. marsh organ experiments) without considering the spatial variation in drainage conditions that occur across a marsh platform (Kirwan and Guntenspergen 2012, Adam Langley et al 2013, Kirwan and Guntenspergen 2015, Janousek et al 2016, Janousek et al 2020, McLain et al 2020, Payne et al 2021). Furthermore, numerical models of marsh vulnerability to accelerated SLR seldom incorporate drainage conditions or subsurface hydrology into the current framework of a dynamic marsh surface elevation that is driven by the feedback between elevation, tide, plant growth and sediment deposition (Kirwan and Murray 2007, L. et al 2010, Marani et al 2013, Mariotti and Carr 2014, D’Alpaos and Marani 2016, Mariotti 2016, Duran Vinent et al 2021).…”