HydrometJanuary 2001 -- AMS Short Course on Instrumentation1 HydrometeorologicalMeasurements Melanie...

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Hydromet January 2001 -- AMS Short Course on Instrumentation

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Hydrometeorological Hydrometeorological MeasurementsMeasurements

Melanie A. Wetzel Desert Research Institute

University of Nevada, Renoand

Hydromet January 2001 -- AMS Short Course on Instrumentation

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Components of the Hydrologic Cycle

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Processes of Transport and TransformationWater resources distribution is controlled by the radiation balance, movement of air masses with contrasting temperature and moisture contents, terrain features and local airflow patterns

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Primary Elements of Hydromet Monitoring

Atmospheric Vapor Cloud Water Rainfall Snowfall Snowpack Groundwater Streamflow Water Quality

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Atmospheric Humidity

Ground-based temperature/humidity monitoring Rawinsondes to provide vapor transport Role of wind-driven evaporation Impact of soil type and other surface parameters

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EvapotranspirationLysimeters measure the loss of water by mass balance from a surface layer usually containing soil and vegetation

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Evaporation

Water loss from open water is a large source of atmospheric moisture. Evaporation from snow in dry or high altitude zones also causes significant loss.

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Measurement of Cloud Water Content

Hot Wire SensorsOptical ProbesImpaction CollectorsCloud Sieves

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Tipping Bucket Raingages

Calibrated per-tip volume is converted to equivalent depth per unit area. Errors due to sticking of snow on sides of funnel, debris, and unrepresentative capture at collection aperture.

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Weighing Bucket and Snow Gages

Use of heating, anti-freeze solutions and apparatus for wind screening improve the measurement of total rain and snow equivalent depths.

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Snow Depth Sensors

Applications which require monitoring of physical snow depth (such as at ski areas) can utilize acoustic snow depth sensors. Amounts are under-represented when snow has a low density due to sound transfer into the snowpack.

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Measurement of Snow Water Equivalent

Snow pillows monitor mass of overlying snow, and snow cores provide column water amount.

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Fuel (Vegetation) Moisture

Fuel Rod devices are designed to simulate moisture content of trees within forest environments, for monitoring fire potential. Fuel moisture is a direct function of atmospheric humidity, precipitation and soil moisture.

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Streamflow Monitoring

Stream discharge is estimated from measurements of the stream stage height.

Stage height instruments:Staff gage

Stilling well / floatBubblerPressure TransducerAcoustic Sensor

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Stream Cross-Sections

Flumes and weirs control flow into a known cross-section, so that river stage height can be monitored visually or automatically. Stage height is related to volumetric discharge using stream profile measurements.

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Current Meters and Profiles

Stream velocity follows a vertical profile similar to boundary layer winds, and measurement depths are selected to according to this profile.

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Discharge Calculations

Number and location of current measurements across the channel are determined from stream width and depth.

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Flood Recurrence Interval

Numerical ranking of peak streamflow is used to estimate the probability of flood conditions.

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Water Quality

Contaminants include sediment, bacteria, metals, aerosols, biogenic chemicals and many others.

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Water Chemistry and Turbidity

Sample collection and automated sensing are used to monitor sediment and pollutant

concentrations.

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Networks of Hydrometeorological Sensors

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Effects of Local ChangesAlterations of the stream channel, soil and vegetation are analogous to modification in the airshed due to construction and urbanization

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ReferencesNathanson, J.A., 1997: Basic Environmental Technology. Prentice

Hall, New Jersey, 440 pp.Ward, A.D., and W.J. Elliot, 1996: Environmental Hydrology.

Lewis, Boca Raton, 496 pp.Watts, S., and L. Halliwell, ed., 1996: Essential Environmental

Science: Methods and Techniques. Routledge, New York, 512 pp.