The
volume of water passing a specific point in a given interval of time is
called streamflow or discharge. Streamflow generally is measured in cubic
meters per
second and most often is determined by measuring the velocity of the water at
a particular cross section of a river. Although streamflow data are more
difficult to collect than stage data, the streamflow data are needed for flood
forecasting and also are needed by many users of water-resource information.
The velocity-area method is the
most common method used to measure streamflow. The method, which is used
by the USGS
and by Ukrainian hydrometeorological staff, requires the physical measurement of the cross
section and of the velocity of the water. The velocity is
measured using a current meter that consists of a propeller that is rotated by
the action of flowing water. Each rotation completes an electrical circuit and
is recorded. The propeller rotation speed depends on the
velocity of the water passing by the propeller.
Streamflow
data for a specific stream location are compared to stage data for that
location and used to develop a rating curve. After the rating curve has been developed, the
streamflow can be estimated from the
curve.
The rating curve for a specific stream
location is developed by making successive streamflow measurements to
define and maintain a stage-streamflow relation. The streamflow measurements and their corresponding stages (or gage
heights) are plotted
on a graph for the stream location. Continuous streamflow throughout the year
then can be determined from the rating curve and the stage record. The
data are checked periodically to ensure accuracy because factors such as ice cover,
debris, and vegetation growth can affect the stage-streamflow relation.
As part of a cooperative agreement among the SWMC, USAID, ULRMC, and USGS, both stage and
streamflow data will be available to all potential users through organization
websites and through published media.