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Hydrology Rainfall - Runoff Modeling (II) Synthetic unit hydrographs

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Hydrology Rainfall - Runoff Modeling (II) Synthetic unit hydrographs Prof. Ke-Sheng Cheng Department of Bioenvironmental Systems Engineering National Taiwan University – PowerPoint PPT presentation

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Title: Hydrology Rainfall - Runoff Modeling (II) Synthetic unit hydrographs


1
HydrologyRainfall - Runoff Modeling
(II)Synthetic unit hydrographs
  • Prof. Ke-Sheng Cheng
  • Department of Bioenvironmental Systems
    Engineering
  • National Taiwan University

2
Synthetic unit hydrographs
  • For areas where rainfall and runoff data are not
    available, unit hydrograph can be developed based
    on physical basin characteristics.
  • SCS unit hydrograph
  • Clarks IUH (time-area method)
  • Linear reservoir model (Nash model)

3
SCS unit hydrograph
4
Misuse of SCS UH an example
5
Clarks IUH (time-area method)
  • The concept of isochrones
  • Isochrones are lines of equal travel time. Any
    point on a given isochrone takes the same time to
    reach the basin outlet. Therefore, for the
    follwoing basin isochrone map and assuming
    constant and uniform effective rainfall,
    discharge at the basin outlet can be decomposed
    into individual contributing areas and rainfalls.

6
Contributing area and contributing rainfall
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  • Using the basin isochrone map, the cumulative
    contributing area curve can be developed. The
    derivatives or differences of this curve
    constitute the instantaneous unit hydrograph
    IUH(t).

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  • If the effect of watershed storage is to be
    considered, the unit hydrograph described above
    is routed through a hypothetical linear reservoir
    with a storage coefficient k located at the
    watershed outlet.
  • For a linear reservoir with storage coefficient
    k, we have

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  • Consider the continuity of the hypothetical
    reservoir during a time interval ?t.

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  • Example. A watershed of 1000-acre drainage area
    has the following 15-minute time-area curve. The
    storage coefficient k of the watershed is 30
    minutes. Determine the 15-minute unit hydrograph
    UH(15,t).

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  • Area between isochrones t 0 and t 0.25 hr is
    100 acres. Since we are interested in the unit
    hydrograph UH(15-min, t), the rainfall intensity
    in the time period (0.25 hr) should be 4 inch/hr.
    Therefore, the ordinate of UH(15-min, t) at time
    t 0.25 hr is
  • 4 inch/hr ? (1/12 ft/inch) ? (1/3600 hr/sec) ?
    100 acres ? (43560 ft2/acre) 403.33 cfs

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Hydrological Analysis for Detention Pond Design
in Hillslope Development
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    ?(Rational Formula)??????????

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