FLOODSCx | |
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Hydrologic Process |
Code
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Comment (text file of 3 lines) |
0
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Subarea Runoff Hydrograph | |
a. Standard Unit Hydrograph Analysis |
1
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b. Small Area Unit Hydrograph (1-min. computation interval only) |
1.1
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Flow-by Basin Analysis | |
a. Hydrograph Separation based on a Constant Q |
2.1
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b. Hydrograph Separation based on a Qinflow vs. Qoutflow Relationship |
2.2
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Flow-Through Basin Analysis | |
a. Modified Puls Method using 5-min. Computation Interval |
3.1
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b. Modified Puls Method using 1-min. Computation Interval |
3.2
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c. Finite Difference Method using 1-min. Computation Interval |
3.3
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Pipe Flow Routing (Kinematic Wave Analog) |
4
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Open Channel Routing Methods | |
a. Translation Method |
5.1
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b. Convex Routing Method |
5.2
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c. Muskingum Routing Method |
5.3
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Set a Stream to Zero |
6
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Add Stream to Another Stream |
7
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Split Hydrograph by Proportioning |
8
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Advance Hydrograph in Time |
9
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Runoff Hydrograph Memory Function | |
a. User-Defined Runoff Hydrograph |
10
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b. Write Stream Hydrograph to a DNA File |
10.1
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c. Read DNA File and add to a Stream |
10.2
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View Stream Hydrograph |
11
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Other Options | |
Metric FLOODSCx: Flood Routing Applications This application incorporates the Unit Hydrograph System Program (UNITHxx) into a high-speed, completely user-interactive watershed simulation computer program. Analogous to the Rational Method Hydrology Program (RATxx), the watershed is split into several subareas by the designer. The watershed can also be divided into streams which are analyzed independently. The study proceeds in a sequential manner (for each stream) in the downstream direction. The designer selects from a menu of possible hydrologic and hydraulic processes to describe the watershed characteristics. With these several submodels, a watershed can be modeled as a link-node system composed of large subareas contributing runoff at nodal points which are linked together by channel or pipe routing submodels. The program also includes several submodels which approximate the important effects of detention basin storage for both flow-through and flowby detention basin processes. These storage approximations allow the runoff hydrograph modeling approach to be used for most complex urban watershed flood control systems, and enables the designer to optimize the necessary flood control benefit to cost ratio.
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