Lecture 6 - Streamflow Flashcards
The flow of water in an open channel (or discharge) is defined as the volume of water passing a specified point in a given interval of time
Streamflow
The ————from a particular watershed can be measured at a particular gauging station by measuring the stage at the station and then converting the stage to an associated discharge using a rating curve.
Streamflow
generally measured by observing stage or elevation above a specified datum, in a channel and then relating stage to discharge via a rating curve.
Streamflow
are plots of water level vs. discharge.
Rating curves
The stage of a river is the height of the water surface above an established reference plane.
Water Stage
Requirements for the Watercourse During Measurement:
The watercourse has to be straight for at least 100 m upstream and downstream from the point of measurement for a regular velocity distribution in the water. No backwater effect. Close to the point of measurement, measurements of velocity have to be near as possible so stage-discharge curves can be compiled.
This gage may consist of a vertical scale attached to a bridge pier, piling, wharf, or other structure that extends into the low-water channel of the stream.
Staff Gage.
Lowered structure surface,
to the and readings are taken as a function of time through a storm event.
Wire-Weight Gage.
Uses a small amount of cork inside an enclosed staff gage. The cork floats as the water rises, and some adheres to the stick at the highest level reached by the water.
Crest Gage.
The only direct system measurement, which can measure the water stage continuously and automatically.
Float Gage.
Used mainly as an inside stilling well reference gage for a water level recorder and consist s of a float attached to a counterweight by means of cable or a stainless steel tape.
Float Gage.
Based on the measurement of pressure needed to produce bubbles against water pressure.
Bubble-Type Pneumatic Gage.
Mainly used when the location is not suitable for a float gage.
Bubble-Type Pneumatic Gage.
Most common method of measuring the stage of a river is through the use of a stilling well.
Stage Height
are located on the bank of a stream or on a bridge pier and are topped by a shelter that holds recorders and other instruments associated with the station.
Stilling wells