Beta version 4 has arrived and Minnesota has new equations for flow durations and low-flow frequencies in version 3
Beta version 4 is now available for most states on a trial basis, and version 3 remains available. Beta version 4 provides a single user interface (at http://streamstatsags.cr.usgs.gov/streamstats/) for all states that are implemented, rather than separate applications for each state, as in versions 2 and 3, and the user interface is more user friendly than previous versions. Information for user-selected ungaged sites currently cannot be obtained using beta version 4 for the States of Arkansas, Arizona, Georgia, Iowa, Indiana, Maryland, North Carolina, Oregon, South Carolina, and Tennessee because of unique functionality for those states that is not yet implemented. Users are encouraged to provide comments and report bugs by use of the Help button on the interface, which also provides access to limited beta version 4 documentation. See below for additional information about versions both 3 and 4.
Please contact the StreamStats by email at firstname.lastname@example.org if you have any questions.
StreamStats version 3 for Minnesota incorporates regression equations for estimating instantaneous peak-flow frequencies, low-flow frequencies and flow durations. The equations for estimating low-flow frequencies and flow durations have not yet been added to version 4 due to current limitations with the software. Equations are available for estimating peak flows with annual exceedance probabilities of 66.7, 50, 20, 10, 4, 2, 1, and 0.002 percent, which correspond to recurrence intervals of 1.5, 2, 5, 10, 25, 50, 100, and 500 years, respectively. In addition, equations are available for estimating annual and seasonal 7-, 30-, and 112-day low flow that recur on average once in 10 years, and for estimating daily streamflows that exceeded between 99.99 and 0.01 percent of the time.
The reports below document the regression equations available in StreamStats version 3 for Minnesota, the methods used to develop the equations and to measure the basin characteristics used in the equations, and the errors associated with the estimates obtained from the equations. Only the peak-flow equations from Lorenz and others (2009) have been implemented in version 4. That report describes the development of a region-of-influence method for estimating peak flows as well as the development of regression equations. StreamStats has not implemented the region-of-influence method. Users should familiarize themselves with both reports before using StreamStats to obtain estimates of streamflow statistics for ungaged sites.
- Lorenz, D.L., Sanocki, C.A., and Kocian, M.J., 2009, Techniques for estimating the magnitude and frequency of peak flows on Small Streams in Minnesota based on data through water year 2005: U.S. Geological Survey Scientific Investigations Report 2009–5250, 54 p.
- Ziegeweid_ J.R._ Lorenz_ D.L._ Sanocki_ C.A._ and Czuba_ C.R._ 2015_ Methods for estimating flow-duration curve and low-flow frequency statistics for ungaged locations on small streams in Minnesota: U.S. Geological Survey Scientific Investigations Report 2015–5170_ 23 p.
General information on the Interactive Map application, as well as specific sources and computation methods for basin characteristics are available here.
Important Note: The streamflow statistics for streamgages used to develop the regression equations from the above reports are not yet available from StreamStats. Users should refer to the tables from those reports to obtain the latest available statistics for the streamgages.
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