Abstract

AbstractThe impact of sea-level rise on salt marsh sustainability is examined for the lower St. Johns River and associated salt marsh (Spartina alterniflora) system. A two-dimensional hydrodynamic model, forced by tides and sea-level rise, is coupled with a zero-dimensional marsh model to estimate the level of biomass productivity of S. alterniflora across the salt marsh landscape for present day and anticipated future conditions (i.e., when subjected to sea-level rise). The hydrodynamic model results show mean low water (MLW) to be highly spatially variable with a SD of ± 0.18 m and mean high water (MHW) to be less spatially variable with a SD ± 0.03 m. The spatial variability of MLW and MHW is particularly evident within the tidal creeks of the salt marsh. MLW and MHW are sensitive to sea-level rise and respond in a nonlinear fashion (i.e., MLW and MHW elevate by an amount that is not proportional to the level of sea-level rise). The coupled hydrodynamic-marsh model results illustrate the spatial hetero...

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