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FS-130-96
U.S. Department of the Interior Gauging Flows in Northeastern Florida Bay
Introduction The South Florida Ecosystem Restoration Program is an intergovernmental effort, involving a number of agencies, to reestablish and maintain the ecosystem of south Florida. One element of the restoration effort is the development of a firm scientific basis for resource decision making. The U.S. Geological Survey (USGS), one of the agencies, provides scientific information as part of the South Florida Ecosystem Restoration Program. The USGS began their own program, called the South Florida Ecosystem Program, in fiscal year 1995 for the purpose of gathering hydrologic, cartographic, and geologic data that relate to the mainland of south Florida, Florida Bay, and the Florida Keys and Reef ecosystems. Management of the south Florida ecosystem involves the use of hydrologic models that simulate the flow of water through the region. As sheetflow is reestablished by flow management in the wetlands of the Everglades, it is expected that changes will also be reflected in the amount of freshwater exiting the mainland through the principal streams or as sheetflow into Florida Bay. Several agencies, including the USGS and the U.S. Army Corps of Engineers (COE), are planning to use hydrologic models to simulate and predict the flows into Florida Bay and the circulation patterns within the bay itself. These models can then be used to determine the effects that management of the inland water system will have on the amount of freshwater the bay receives from the mainland. This project will provide modelers with essential flow and specific conductance data along the mangrove zone where data have not been previously available.. Project Goal The objective of this project is to provide hydrologic modelers with information on flow and specific conductance at key outflow points (streams) along the mangrove zone in northeastern Florida Bay(fig. 1). Monthly water samples for "total" nutrient analysis will be collected to complement work by other agencies and to determine possible trends. Additionally, various field data collection and data analysis techniques will be explored to determine the most suitable technique for gauging flows in the shallow and slow-moving estuarine streams that discharge into Florida Bay. Background
Flow through the mangrove zone in northeastern Florida Bay is naturally controlled by the wet or dry conditions of the Everglades wetlands, regional wind patterns and, to some extent, by tidal action in the Gulf of Mexico toward the western part of the bay. The flow of freshwater from the mainland into northeastern Florida Bay is mostly confined to several streams or creeks, except during extreme high-water conditions when significant sheetflow can also be observed through low-lying mangrove areas between the streams. Gauging surface-water flows using acoustic technology has been in practice for some time and is considered to be the most suitable method for measuring water velocities in streams that discharge water into Florida Bay. Research Plan Eight sites located in Terrapin Bay and Long Sound will be studied in northeastern Florida Bay (fig. 1). These sites are: McCormick Creek (1), Taylor River (2), East Creek (3), Mud Creek (4), Trout Creek (5), a small unnamed creek (6), West Highway Creek (7), and East Highway Creek (8). Activities at these sites will include the collection of continuous water-level and velocity data with periodic field measurements of discharge. Five of the eight sites (1, 2, 4, 5, and 7) will be equipped with the following instruments for the continuous collection of field data: acoustic velocity meters (AVM's) to record water velocities at predetermined elevations within the water column, water-level recorders for the calculation of stage dependent cross-sectional areas, temperature and specific conductance sensors, and data collection platforms (DCP's) for the transmission of all data to the USGS office in Miami for processing and storage. A sketch of the vertical and horizontal instrument configurations is shown in figure 2. Velocities and specific conductance will be recorded at three different elevations with temperature only recorded at top and bottom elevations. Periodic measurements of discharge will be made at East Creek (3) in Little Madeira Bay and also at East Highway Creek (8) and a small unnamed creek (6), both in Long Sound. All discharge measurements will be performed using an Acoustic Doppler Current Profiler (ADCP). Discharge records for all instrumented sites will be calculated by the use of stage dependent cross-sectional areas and relations established between AVM recorded velocities and mean measured velocities (ADCP). Water samples for nutrient analysis (nitrogen and phosphorus) will be collected on a monthly basis at all five instrumented sites. One vertically integrated sample will be collected for each site at a point near the center of the stream. In the event that bidirectional flow is observed at the time of sampling, two additional samples will be taken, one near the water surface and the other near the streambed.
Product Plans
Project Schedule Dates and project activities are summarized below. For those project activities that have not yet begun or have not been completed, tentative dates are given. By Eduardo Patino
For more information contact:
Eduardo Patino Related information:
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U.S. Department of the Interior, U.S. Geological Survey
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Last updated: 22 May, 2007 @ 10:53 AM(TJE)
