1 / 17

Streamflow Estimation

Streamflow Estimation. Module 8.6. How do we estimate flow where no gauge exists?. Particularly pertinent question Where gauge existed, use correlation Relationship may not be valid in areas of extensive landcover modification Estimate based on hydrologic similarity

Download Presentation

Streamflow Estimation

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript


  1. Streamflow Estimation Module 8.6

  2. How do we estimate flow where no gauge exists? • Particularly pertinent question • Where gauge existed, use correlation • Relationship may not be valid in areas of extensive landcover modification • Estimate based on hydrologic similarity • Roughly the same volume of flow per unit area will be generated from hydrologically homogeneous areas • Manning’s Equation !! • Useful for design purposes

  3. Manning’s Equation For uniform flow in a channel: Where:v = average velocity (ft s-1)R = hydraulic radius of channel (ft)S = slope of channel (dimensionless)n = Manning’s roughness coefficient Note: in SI units, replace 1.5 by 1 !!

  4. d w Manning’s Equation Hydraulic Radius of Channel: R = A/P Where: A is the cross sectional area P is the wetted perimeter Why use wetted perimeter and not total perimeter? Estimate from geometrical relationships, or surveyedcross section

  5. Manning’s Equation Hydraulic Radius of Channel: R = A/P Slope of Channel: S = drop / distance drop distance Estimate from topographic maps, or survey stream reach

  6. Manning’s Equation Hydraulic Radius of Channel: R = A/P Slope of Channel: S = drop / distance • Finally we must estimate Manning’s n • range: 0.01 (concrete) – 0.1 (coarse bed, dense brush) • n depends on: • bed material, vegetation, channel configuration, sinuosity • varies with stage • Herein lies the true art of the method !!

  7. Palouse River at Colfax: n @ 0.01

  8. Columbia River at Vernita: n = 0.024

  9. Clearwater at Kamiah: n = 0.033

  10. Spokane River at Spokane: n = 0.038

  11. Grande Ronde at LaGrande: n = 0.043

  12. SF Clearwater at Grangeville: n = 0.05

  13. Boundary Creek at Porthill: n = 0.073

  14. Ötz near Ötz Village : n = 0.12?

  15. Red River near Elk City: n = ?

  16. Paradise Creek near CNR: n = ?

  17. Example 10 ft. 50 ft. Estimate bankfull flow…

More Related