Software for Engineers

Skip Navigation LinksEngenious > StormShed3G > 3GDocs > Runoff/Precipitation > SBUH
Skip Navigation Links
Home
StormShed2G
2GNote
Feature List
2G Documentation
2G Online TutorialExpand 2G Online Tutorial
StormShed3G
Whats New
3GDocsExpand 3GDocs
Video Training
Installation
HSPF ToolKit
ToolKit Introduction
ToolKit Features
ToolKit Requirements
ToolKit Installation
Using a Black Box?
Video Training
Misc Product InfoExpand Misc Product Info
Technical
WSDOT Tech Note 3
FAQ
Licensing
Pricing
Updates
Contact
Server Status

Santa BarbaraUrban Hydrograph

The discussion on this methodology is adapted from the King County Surface Water Design Manual, 1994, King County Washington. The Santa Barbara Urban Hydrograph (SBUH) was developed by the Santa Barbara Flood Control and Water Conservation District in California as a short cut to the SCS Unit hydrograph. The primary difference between the SBUH and the SCSUH method is the use of the unit hydrograph in computing the runoff hydrograph. The SBUH replaces the unit hydrograph with an algorithm. The SBUH method greatly simplifies the computation of runoff hydrographs.

The SBUH uses two (2) steps to synthesize the runoff hydrograph.

  1. Computing the instantaneous hydrograph
  2. Computing the runoff hydrograph

The instantaneous hydrograph, It, in cfs, at each time step, dt is computed as follows:

I=60.5RA/dt

Where

  • Rt=total runoff depth at time increment dt (inches).
  • A=area in acres
  • dt=time interval in minutes.

The runoff hydrograph, Qt, is then obtained by routing the instantaneous hydrograph It through an imaginary reservoir with a time delay equal to the time of concentration, Tc of the drainage basin. The following equation estimates the routed flow, Qt. SBUH Routing equation Where W=dt/(2Tc+dt) dt = time interval in minutes.

Spreadsheet format for SBUH Method

ColumnDescription
Column 1Time step number. This is column starting with zero (0) and incrementing by one (1).
Column 2Time in minutes. For a time step of 10 minutes, the column would increment from zero (0) , 10, 20, 30 etc.
Column 3Rainfall distribution as a % of the total precipitation.
Column 4Incremental rainfall (inches). This is just the total precipitation times column 3. Be sure to divide by 100, since column 3 is in %
Column 5Accumulated Rainfall (inches). Just sum the previous column. We should make a comment about columns 3, 4 and 5. Generally, the rainfall distribution is provided as an accumulated distribution, meaning at time zero, there is zero rainfall and at the last time step, the rainfall is one (1) or 100% accumulated. If that is the case, column 3 can be omitted, column 4 can be the accumulated rainfall ratio and column 5, this column can just be the total precipitation multiplied by the column 4.
Column 6Accumulated Runoff. This column checks to see if the Column 5 is less than 0.2s. If it is, then zero (0) is returned, otherwise the abstraction is return.
Column 7Incremental Runoff. Just subtract the previous column 6 from this column 6.
Column 8Total Runoff. This should be the same as column 7 unless there are several areas that are being combined. In which case, it is the sum of the column 7 of each of those areas.
Column 9Instant Hydrograph. This is where the SBUH method diverges from the SCSUH method. For the SBUH method, we just apply the equation:Where A is the total project area and dt is the time increment.
Column 10Design Hydrograph. We apply the remainder of the SBUH method equation:
Page Maintained by Engenious Systems, Inc.