Abstract Coastal forests are increasingly vulnerable to climate change and sea‐level rise, with flooding and salinity driving transitions to marsh‐dominated ecosystems. Using the coastal version of FATES‐Hydro, we conducted 30‐year simulations at two coastal forest sites—a broadleaf swamp white oak stand at Lake Erie and a conifer loblolly pine stand at Chesapeake Bay—under historical climate and elevated CO 2 (+100 ppm) and temperature (+1.5°C) scenarios. Elevated CO 2 increased net primary productivity at both sites, while warming alone intensified hydraulic stress and accelerated mortality, particularly in the conifer stand. Simulations show that elevated temperatures intensify vapor pressure deficit and hydraulic stress on trees already experiencing salinity‐ and submersion‐driven water stress, increasing tree mortality beyond what would be expected in a non‐water‐limited environment. Marsh expansion partially compensated for tree loss at the Lake Erie site but reduced ecosystem productivity in the conifer forest at Chesapeake Bay. Our results highlight how differences in stand structure, phenology, and local hydrology modulate ecosystem trajectories under climate change, emphasizing the importance of demographic and community‐level processes for predicting the fate of coastal forests.
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Junyan Ding
Nate G. McDowell
Nathan Conroy
Journal of Geophysical Research Biogeosciences
Los Alamos National Laboratory
Argonne National Laboratory
Oak Ridge National Laboratory
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Ding et al. (Wed,) studied this question.
www.synapsesocial.com/papers/69d8948f6c1944d70ce0574b — DOI: https://doi.org/10.1029/2025jg009305