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Welcome to StreamStats

Kentucky

Beta Version 3 is now available for Kentucky with new equations

New regression equations were added to the StreamStats version 3 application for Kentucky on August 26, 2015. In addition to the peak-flow equations that were available previously, equations for estimating low-flow frequency statistics, mean annual flows, and harmonic mean flows, as well as bankfull flow, area, width, and depth are now available.

Currently, version 3 can only delineate drainage basins, compute basin characteristics, and estimate streamflow statistics using regression equations for user-selected sites. It also can provide reports of information for USGS data-collection stations. All other functionality that previously was available in version 2 will be added to version 3 as quickly as possible, with a goal of having all functionality available by the end of 2015.

Please help us conserve our server system resources by closing the Interactive Map window when you are finished using it. Doing so will help ensure system availability for all users. Thank you.

Also, please bookmark this page rather than the Interactive Map page, as the URL for the interactive map may change in the future.

Kentucky StreamStats incorporates regression equations for estimating instantaneous peak flows with annual exceedance probabilities of 50, 20, 10, 4, 2, 1, 0.5, and 0.2 percent. These peak flows have recurrence intervals of 2, 5, 10, 25, 50, 100, 200, and 500 years, respectively. Equations for estimating mean annual flows, harmonic mean flows, and the 7-day 2-, 10-, and 20-year and 30-day 2- and 5-year low flows also are included. In addition, Kentucky StreamStats include equations for estimating bankfull flow, area, width, and depth. The reports below document the regression equations available in StreamStats for Kentucky, 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. Users should familiarize themselves with these reports before using StreamStats to obtain estimates of streamflow statistics for ungaged sites.

The peak-flow regression equations are implemented only for hydrologic regions 2, 3, 5, 6, and 7 in Kentucky. Drainage area is the only explanatory variable in these equations. Equations for hydrologic regions 1 and 4 are not implemented at this time because an additional explanatory variable, stream slope, is needed to solve the equations. The capability for StreamStats to compute stream slope in a manner that duplicates the method used in the report by Hodgkins and Martin (2003) has not yet been devised.

 

Interactive Map

 

General information on the Interactive Map application, as well as specific sources and computation methods for basin characteristics are available here.

StreamStats for Kentucky was developed in cooperation with the Kentucky Energy and Environment Cabinet, Department of Environmental Protection, Division of Water.

Link to Kentucky Energy and Environment Cabinet, Department of Environmental Protection

Contact Us if you experience any problems with this application.






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