No abstract

The south-eastern United States and Gulf Coast of Mexico is physiographically diverse, although dominated by a broad coastal plain. Much of the region has a humid, warm temperate climate with little seasonality in precipitation but strong seasonality in runo owing to high rates of summer evapotranspiration. The climate of southern Florida and eastern Mexico is subtropical with a distinct summer wet season and winter dry season. Regional climate models suggest that climate change resulting from a doubling of the pre-industrial levels of atmospheric CO 2 may increase annual air temperatures by 3±48C. Changes in precipitation are highly uncertain, but the most probable scenario shows higher levels over all but the northern, interior portions of the region, with increases primarily occurring in summer and occurring as more intense or clustered storms. Despite the increases in precipitation, runo is likely to decline over much of the region owing to increases in evapotranspiration exceeding increases in precipitation. Only in Florida and the Gulf Coast areas of the US and Mexico are precipitation increases likely to exceed evapotranspiration increases, producing an increase in runo. However, increases in storm intensity and clustering are likely to result in more extreme hydrographs, with larger peaks in¯ow but lower base¯ows and longer periods of drought.The ecological eects of climate change on freshwaters of the region include: (1) a general increase in rates of primary production, organic matter decomposition and nutrient cycling as a result of higher temperatures and longer growing seasons: (2) reduction in habitat for cool water species, particularly ®sh and macroinvertebrates in Appalachian streams; (3) reduction in water quality and in suitable habitat in summer owing to lower base¯ows and intensi®cation of the temperature±dissolved oxygen squeeze in many rivers and reservoirs; (4) reduction in organic matter storage and loss of organisms during more intense¯ushing events in some streams and wetlands; (5) shorter periods of inundation of riparian wetlands and greater drying of wetland soils, particularly in northern and inland areas; (6) expansion of subtropical species northwards, including several non-native nuisance species currently con®ned to southern Florida; (7) expansion of wetlands in Florida and coastal Mexico, but increase in eutrophication of Florida lakes as a result of greater runo from urban and agricultural areas; and (8) changes in the¯ushing rate of estuaries that would alter their salinity regimes, strati®cation and water quality as well as in¯uence productivity in the Gulf of Mexico.Many of the expected climate change eects will exacerbate current anthropogenic stresses on the region's freshwater systems, including increasing demands for water, increasing waste heat loadings and land use changes that alter the quantity and quality of runo to streams and reservoirs. Research is needed especially in several critical areas: long-term monitoring of key hydrological, chemical and biologi...

Fire followed by flooding has been observed to reduce stand density greatly or kill large stands of sawgrass (Ctadiumjamaicense Crantz). Nonetheless sawgrass is the dominant plant in the marshes of the Everglades in southern Florida, where lightning fire occurs during the season when the likelihood of flooding immediately after fire is greatest. Sawgrass regrowth was observed after three different fires (two caused by lightning and one set by managers) under different hydrologic conditions in order to determine how sawgrass survives in a regime where fires occur at the same time of year as rapidly rising water. Mean sawgrass leaf elongation rates were found to be less than the mean rate of water-level increase during May and June, suggesting that s awgrass could not survive solely by outgrowing rising water. Remnant culms were usually 8 to 14 cm above water level immediately post fire, equivalent to approximately 10 days regrowth. This 'headstart' on growth reduced the probability of widespread death due to flooding by about half during the period when lightning fires were most common.