WMS:TR-55 Hydrographs: Difference between revisions

From XMS Wiki
Jump to navigationJump to search
Line 13: Line 13:
WMS uses exhibit 5 in the TR-55 manual for the tabular hydrograph method.
WMS uses exhibit 5 in the TR-55 manual for the tabular hydrograph method.


Values for the <math>T_c</math>, <math>T_t</math>, <math>I_a/P</math>, and <math>A_m*Q</math> are used as input values for this table, and all hydrograph values are linearly interpolated or extrapolated from the values for <math>T_c</math>, <math>T_t</math>, and <math>I_a/P</math>.  The difference between the WMS method and the method described in the manual is the WMS hydrograph is linearly interpolated.  The method described in the manual just rounds the values for <math>T_c</math>, <math>T_t</math>, and <math>I_a/P</math>.  So you should basically get the same results, but the WMS results will be more accurate and can go beyond the minimum and maximum values for <math>T_c</math>, <math>T_t</math>, and <math>I_a/P</math> (this is not recommended).
Values for the <math>T_c</math>, <math>T_t</math>, <math>I_a/P</math>, and <math>A_m*Q</math> are used as input values for this table, and all hydrograph values are linearly interpolated or extrapolated from the values for <math>T_c</math>, <math>T_t</math>, and <math>I_a/P</math>.  The difference between the WMS method and the method described in the manual is the WMS hydrograph is linearly interpolated.  The method described in the manual just rounds the values for <math>T_c</math>, <math>T_t</math>, and <math>I_a/P</math>.  So users should basically get the same results, but the WMS results will be more accurate and can go beyond the minimum and maximum values for <math>T_c</math>, <math>T_t</math>, and <math>I_a/P</math> (this is not recommended).


==Related Topics==
==Related Topics==

Revision as of 16:02, 12 September 2014

Using the TR-55 tabular hydrograph method (see TR-55 reference manual for details), hydrographs for a selected basin or outlet may be computed. The Compute Hydrograph(s) button is chosen once all of the necessary input for basins and outlets have been entered and a new set of hydrographs will be computed.

If you have a basin selected when you compute hydrographs, then a hydrograph for only the selected basin will be computed. However, if you have an outlet selected when you compute hydrographs, then a new hydrograph for each upstream basin will be computed along with the routed hydrographs at outlet points.

You may notice a slight difference between hydrographs computed by WMS-TR-55 implementation and those in the TR-55 reference manual. This difference occurs because the Failed to parse (SVG with PNG fallback (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://en.wikipedia.org/api/rest_v1/":): {\displaystyle I_a/P} value is rounded to the nearest hydrograph value for the standard version of TR-55. In WMS hydrographs are determined by linear interpolation between two hydrographs using the actual Failed to parse (SVG with PNG fallback (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://en.wikipedia.org/api/rest_v1/":): {\displaystyle I_a/P} value.

Information about discrepancies between the TR-55 Hydrograph peak flow values and the Unit Peak Discharge method peak flow values

One question that is frequently asked about TR-55 hydrographs is why the peak flow computed from the TR-55 unit peak discharge method is different from the peak flow on the TR-55 computed hydrograph. Though the TR-55 tabular hydrograph method, which is used to compute TR-55 hydrographs, may give similar results to the TR-55 unit peak discharge method, which is used to compute a peak flow, the peak flows from these two different methods will usually be different. WMS uses the method described in Exhibit 5 in the TR-55 manual to compute a hydrograph using the tabular hydrograph method. Hydrograph ordinates used in the the TR-55 tabular hydrograph method were originally obtained from a series of TR-20 runs with different times of concentration and other values, as described in the TR-55 manual. See the TR-55 manual for more information.

Additional Information

WMS uses exhibit 5 in the TR-55 manual for the tabular hydrograph method.

Values for the Failed to parse (SVG with PNG fallback (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://en.wikipedia.org/api/rest_v1/":): {\displaystyle T_c} , Failed to parse (SVG with PNG fallback (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://en.wikipedia.org/api/rest_v1/":): {\displaystyle T_t} , Failed to parse (SVG with PNG fallback (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://en.wikipedia.org/api/rest_v1/":): {\displaystyle I_a/P} , and Failed to parse (SVG with PNG fallback (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://en.wikipedia.org/api/rest_v1/":): {\displaystyle A_m*Q} are used as input values for this table, and all hydrograph values are linearly interpolated or extrapolated from the values for Failed to parse (SVG with PNG fallback (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://en.wikipedia.org/api/rest_v1/":): {\displaystyle T_c} , Failed to parse (SVG with PNG fallback (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://en.wikipedia.org/api/rest_v1/":): {\displaystyle T_t} , and Failed to parse (SVG with PNG fallback (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://en.wikipedia.org/api/rest_v1/":): {\displaystyle I_a/P} . The difference between the WMS method and the method described in the manual is the WMS hydrograph is linearly interpolated. The method described in the manual just rounds the values for Failed to parse (SVG with PNG fallback (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://en.wikipedia.org/api/rest_v1/":): {\displaystyle T_c} , Failed to parse (SVG with PNG fallback (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://en.wikipedia.org/api/rest_v1/":): {\displaystyle T_t} , and Failed to parse (SVG with PNG fallback (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://en.wikipedia.org/api/rest_v1/":): {\displaystyle I_a/P} . So users should basically get the same results, but the WMS results will be more accurate and can go beyond the minimum and maximum values for Failed to parse (SVG with PNG fallback (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://en.wikipedia.org/api/rest_v1/":): {\displaystyle T_c} , Failed to parse (SVG with PNG fallback (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://en.wikipedia.org/api/rest_v1/":): {\displaystyle T_t} , and Failed to parse (SVG with PNG fallback (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://en.wikipedia.org/api/rest_v1/":): {\displaystyle I_a/P} (this is not recommended).

Related Topics