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National Capital Region Network


National Capital Region Network - Monitoring Surface Water Dynamics

Background

Surface Water Dynamics describe the quantity and movement of water in a surface body such as a stream or lake. They include flow or discharge for flowing waterbodies and stage or level for non-flowing waterbodies To satisfy a variety of ecological uses (fish and other aquatic organisms, terrestrial wildlife, riparian and channel vegetation, recharge groundwater) a stream or other body of water should have sufficient quantity and quality of water for every day of the year. Height of stream flow varies seasonally under natural conditions; however any extreme variation can be stressful to organisms and damaging to the physical environment. Urban areas have a large number of impervious surfaces such as parking lots, streets, sidewalks, and buildings. Impervious surfaces reduce groundwater recharge and baseflow into streams because less water percolates into the soil, and increase the velocity and amount of runoff into lakes, rivers, and streams through overland flow, storm drains, and sewer outfalls.

The intensity of the exposure to potential stressors for stream organisms depends on how fast water is traveling past the organisms, and on the dilution factor, which depends on how much water is in the stream. Surface water dynamics data provides key support data for other vital signs indicators including freshwater quality, groundwater dynamics, stream threatened and endangered (T&E) species and fish assemblages, T&E amphibians and reptiles, erosion and deposition, wetlands, and riparian habitat.

Links
Reports

  • Contacts
    Marian Norris
    NCRN Water Resources Specialist
    202.342.1443 ext. 206
    NCRN Stream Monitoring

    Objectives

    • Monitor the flow volume (discharge) of surface water in major streams of the NCRN parks.
    • Assess the availability of sufficient water for ecological, recreational, and aesthetic purposes of the parks.
    • Develop rating curves for a range of environmental conditions, land use, and weather patterns, for each water body (e.g., compare a drought year vs. an El NiƱo year) in order to gain an overall understanding of hydrologic systems within the NCRN.
    • Determine seasonal and annual trends.
    • Provide support data for other Vital Signs indicators in order to help understand trends in aquatic species populations, pollution transport, erosion/deposition, and other natural processes and features.
    • Share data with state and local groups for TMDL and other regulatory decision purposes.

    Measures

    A continuous record of stage is obtained by installing instruments that sense and record the water-surface elevation in the stream. Discharge measurements are initially made at various stages to define the relation between stage and discharge. Discharge measurements are then made at periodic intervals, usually monthly, to verify the stage-discharge relation or to define any change in the relation owing to changes in channel geometry. An analysis of the manner in which discharge varies over time, or the hydrograph, allows a lotic scientists to examine the characteristics of the watershed that influence such conditions as runoff and storage. A hydrograph can be plotted from gauging records to display yearly, monthly, daily, or instantaneous discharges. A hydrograph can also provide information on daily and monthly total flow, mean monthly discharge, base (often groundwater maintained) flow, stage height, and periods of high and low flow.

    Status

    The Water Resources Specialist and Hydrologic Technician collect flow, stream width, and depth data monthly from every sampling site. Several sites also have continuous water level loggers installed.

    Last updated: December 3, 2008   I   http://inp2300fcsdepo1.nps.doi.net/im/units/ncrn/monitoring_water_surface_dynamics.cfm   I  Email: Webmaster
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