- About AL
- Research at AL
- Aquatic Ecology
- Behavioral and Evolutionary Ecology
- Conservation & Restoration Ecology
- Landscape Ecology
- Comparison of species- and community-level models across novel climates and communities
- Plant Community Response to Changes in Water
- Using Landsat Time Series Data to Examine Patterns in Water Surface Temperature in the Chesapeake Bay
- Extinction Risk of the Delmarva Fox Squirrel
- Potomac Initiative
- Quantifying Feedbacks in Desert Vegetation
- Remote Sensing and Forest Disturbance
- Medium-resolution Phenology and Forest Productivity
- Biologically-Optimized Environmental Classification of Maryland Streams
- Predicting Vulnerability to Sea Level Rise
- Landscape Controls on Seasonal Timing and Growing Season Length
- Watershed Hydrology and Biogeochemistry
- Acid-Base Status of Western Maryland Streams
- BMP's for Natural Gas Drilling
- Modeling Stream Distribution and Stream Burial in Large River Basins
- Improvements in Surface Water Quality Due to Declining Atmospheric N Deposition
- Land Use Changes on Stormflow Dynamics
- Piney Creek Reservoir Assessment
- Relationship Between Wetlands and Mercury in Brook Trout
- Seminar Series
- Chesapeake Watershed CESU
- Central Appalachians Stable Isotope Facility
- Donate to AL
- Johnson Award
The Potomac Initiative
UMCES researchers have assembled detailed land use, climate and hydrological data for the Potomac basin as the basis for a nested series of spatially explicit models to characterize the response of large watersheds (100-1,000 square km) to the combined effects of climate and land use change.
Large rivers are important
Large river systems, which drain vast areas and transport sediment, nutrients and chemicals over long distances, provide an integrative measure of the impact of social, economic and ecological change at regional scales. The Potomac watershed has a complex mix of land cover types with a dramatic east-west gradient in topography and climate. This basin is experiencing extensive changes in land-use making the Potomac an excellent representative of landscapes being experienced throughout the eastern seaboard of the United States.
Characteristics of the Potomac watershed
The mainstem of the Potomac river is 617 kilometer-long and runs through five geological provinces, draining approximately 37,800 square kilometers of Maryland, Pennsylvania, Virginia, and West Virginia. Over 5.3 million people live within this watershed, with approximately 3.7 million Washington, D.C. area residetns drawing about 1.8 billion liters of water per day from the river. The Potomac is also a major contributor to waters of the Chesapeake Bay, the largest estuary in the United States.
Linking land-use change to watershed effects
The net effect of local, incremental change in land use has important implications for controlling the levels of sediment and nutrient loading to the Potomac. We know that increasing sediment and nutrient concentrations will adversely affect eutrophication, hypoxia, and light availability for biota within the Chesapeake Bay, but prediction of downstream effects in large river systems cannot be obtained by simply summing upstream inputs. We expect that small, cumulative change can lead to sudden declines in water quality and threaten the biotic integrity of these important river systems.
The Potomac provides a model for study because of its setting within a landscape continuum from mountains to the Bay; its geomorphic and land-use diversity; its rapid population growth; and its importance as the primary drinking water supply for the Nation's capital and as habitat for a diverse biota.
We are investigating the impacts of a variety of landscape changes within the Potomac basin, including urbanization, forest disturbance, and surface mining. Documented impacts include acidification of western Maryland streams, increased flooding, altered fish composition and behavior, and increased leakage of nutriends from forests to surface waters. Tools used for these studies include models at multiple spatial scales, paired watershed studies, and remote-sensing landscape analysis.
Climate change and land-use interactions
The effects of climate change on river systems in the eastern United States are difficult to assess because:
- current climate models do not adequately predict the full spectrum of expected weather conditions - especially large storms and extended droughts;
- the fine-scale, detailed response of terrestrial and aquatic ecosystems to changing weather conditions (e.g., earlier phenology, increasing evapotranspiration) have not been systematically explored; and
- the concurrent effects of land-cover and land-use change have not been included within the assessment process.
We are investigating these interactive effects by combining weather estimation tools with fine-scale models of land use and ecosystem change within spatially explicit hydrological models that span mulitple spatial resolutions, from the mid-size watershed scale (100 - 1,000 square km) to a large river basin, the Potomac River (37,800 square km).
Restoration across the terrestrial-aquatic boundary
The Potomac Initiative includes a strong emphasis on understanding the linkages between upland land-use and aquatic systems, including restoration of the terrestrial-aquatic interface. Streams are effective sinks for nutrients and habitat for native species. These features are enhanced wherever flow can rapidly exchange with groundwater within the floodplain. The goal of science is to quantify these linkages under various disturbance regimes (e.g., surface mining, buried streams) and understand the spatial scales under which they are most significant. Likewise the goal of stream restoration is to reconnect stream flow to the floodplain, providing solutions to our most common watershed problems.
- Mark Castro - atmosphere-biosphere interactions
- Andrew Elmore - ecohydrology and remote sensing
- Keith Eshleman - biogeochemical processes and watershed hydrology
- Katia Engelhardt - biodiversity, sustainability and restoration ecology
- Robert H. Gardner - landscape ecology and ecosystem theory
- Robert Hilderbrand - conservation biology of stream ecosystems
- Jason Julian - hydrogeomorphic controls on ecosystem processes
- Raymond P. Morgan - pollution effects on aquatic ecosystems
- Margaret Palmer - stream and ecosystem ecology
- Walt Boynton - coastal marine ecology
- Tom Fisher - terrestrial and atmospheric nutrient dynamics
- Larry Sanford - sediment transport mechanics in coastal and estuarine ecosystems
- Jeff Cornwell - sediment biogeochemistry in estuaries and coastal wetlands
- Victoria Coles - physical oceanography and climate change effects
- Bill Dennison - ecosystem health and sustainability