Abstract. Shaped by the hydrology of the Kissimmee-Okeechobee-Everglades watershed, the Florida Everglades is composed of a conglomerate of wetland ecosystems that have varying capacities to sequester and store carbon. Hydrology, which is a product of the region's precipitation and temperature patterns combined with water management policy, drives community composition and productivity. As shifts in both precipitation and air temperature are expected over the next 100 years as a consequence of climate change, CO 2 dynamics in the greater Everglades are expected to change. To reduce uncertainties associated with climate change and to explore how projected changes in atmospheric CO 2 concentration and climate can alter current CO 2 exchange rates in Everglades freshwater marsh ecosystems, we simulated fluxes of carbon among the atmosphere, vegetation, and soil using the DAYCENT model. We explored the effects of low, moderate, and high scenarios for atmospheric CO 2 (550, 850, and 950 ppm), mean annual air temperature (þ1, þ2.5, and þ4.28C) and precipitation (À2, þ7, and þ14%), as predicted by the IPCC for the year 2100 for the region, on CO 2 exchange rates in short-and long-hydroperiod wetland ecosystems. Under 100 years of current climate and atmospheric CO 2 concentration, Everglades freshwater marsh ecosystems were estimated to be CO 2 -neutral. As atmospheric CO 2 concentration increased and under climate change projections, there were slight shifts in the start and length of the wet season (À1 to þ7 days) and a small enhancement in the sink capacity (by À169 to À573 g C m À2 century À1 ) occurred at both short-and longhydroperiod ecosystems compared to CO 2 dynamics under the current climate regime. Over 100 years, rising temperatures increased net CO 2 exchange rates (þ1 to 13 g C m À2 century
À1) and shifts in precipitation patterns altered cumulative net carbon uptake by þ13 to À46 g C m À2 century
À1. While changes in ecosystem structure, species composition, and disturbance regimes were beyond the scope of this research, results do indicate that climate change will produce small changes in CO 2 dynamics in Everglades freshwater marsh ecosystems and suggest that the hydrologic regime and oligotrophic conditions of Everglades freshwater marshes lowers the ecosystem sensitivity to climate change.