WMS:NSS Computing Peak Discharges

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National Flood Frequency Regression Method dialog

Setting up the analysis consists of the following steps, all done within the National Streamline Statistics Method dialog. The dialog can be used to do the follow:

  1. Delineate the watershed and compute the basin area and other geometric parameters. Enter the value manually if not having delineated from a DEM, drainage coverage, or TIN.
  2. Select the State the watershed is in and assign the Maximum Flood Region.
  3. Select the region equation that the watershed is in and while highlighted from the Available Equations window choose the Select button so that it will be listed in the Selected Equations window. If the watershed overlaps more than one region then select the other regions as well.
  4. Variable values derived from a DEM or Drainage coverage will automatically be placed in the appropriate edit fields. Other variables not computed will need to be defined.
  5. Select the Compute Results button to estimate the peak flows for the 2, 5, 10, 25, 50, 100 and 500-year recurrence intervals.

A hydrograph can be estimated by selecting one of the peak flow rows from the Results table and choosing the Compute Hydrograph button.

National Streamline Statistics Method Dialog Overview

The dialog is divided into four sections: Basin Information, Regional regression equations, Variable Values, and Results.

Basin Information

  • Basin Name

Displays the basin ID by default. A different name can be manually entered if desired.

  • Total Basin Area

The total basin area includes the area of all regions overlapped by the watershed. If a terrain model is used to compute areas, this value will be defaulted to the area computed for the selected basin.

  • State

The NSS regression equations are separated by state. The State drop down menu is used to specify the state that the watershed is located in. Once the state is specified, the available regions will appear in the regional equations text window. Besides the 50 US states, an equation for Puerto Rico and a custom defined equation can be selected from the available choices.

  • Max Flood Region

For comparison and evaluation, the NSS program compares each extrapolated 500-year flood peak discharge with the maximum flood-envelope curves given by Crippen and Bue (1977) and Crippen (1982). The map below shows the different flood regions, and should be used to determine the appropriate region for the watershed. A default value has been determined for each region, but this value may be overwritten.

  • Units

Units can be displayed in either "English" or "Metric".

Map showing maximum flood regions in the United States

Regional Regression Equations

Each state is divided up into hydrologically similar regions with separate regression equations. Once the state is selected, the available regions appear in this section of the dialog.

  • Available Equations
  • Selected Equations
  • Select→
  • ←Remove
  • Compute Overlapping Areas

Variable Value

  • Restore Computed Geometric Values

Overrides defaulted values and returns to the computed values.

Results

  • Weighting Options
  • Compute Results

Estimate the peak flows for the 2, 5, 10, 25, 50, 100 and 500-year recurrence intervals.

  • Max Flood Envelope
  • Compute Hydrograph

A hydrograph can be estimated using the dimensionless hydrograph derived by the NSS program once peak flows have been computed. When computing a hydrograph a lag time must be defined. The lag time can be computed using either of the available methods in WMS, or by entering it manually.

  • Export

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