Development of a Hydrologic Model and Estimation of its Parameters Francisco Olivera, Ph.D., P.E. Department of Civil Engineering Texas A&M University
Dec 20, 2015
Development of a Hydrologic Model and Estimation of its Parameters
Francisco Olivera, Ph.D., P.E.Department of Civil Engineering
Texas A&M University
Hydrologic Parameters
Watershed
Abstractions and routing method
Parameters
Stream
Routing method
Parameters
Watershed Abstractions
Precipitation (mm/hr)
Excess precipitation (mm/hr)
Excess precipitation = f(Precipitation, Terrain properties)
Terrain properties
Watershed Abstractions
SCS curve number method
10
CN1000
8.0P
10CN
10002.0P
P
2
e
Pe: cumulative excess precipitation (in)P: cumulative precipitation (in)CN: parameter of infiltration (curve number)
Watershed Abstractions
Initial plus constant loss rate
Pe: cumulative excess precipitation (mm)P: cumulative precipitation (mm)Iloss: initial loss (mm)Closs: constant loss rate (mm/hr)t - t0: time since the beginning of the storm (hrs)
)tt(CI)t(P)t(P 0losslosse
Watershed Routing
Excess precipitation (mm/hr)
Flow (m3/s)
Watershed
Flow = f(Excess precipitation, Watershed geomorphology)
Watershed Routing
Excess precipitation (mm/hr)
Flow (m3/s)
Time
Exce
ss
pre
cipi t
ati
on
Flow
tp
SCS unit hydrograph
tp: watershed lag-time (min)
Watershed Lag-Time (SCS)
t5.3,
S67.31
]9)CN/1000[(Lmaxt
5.0
7.08.0w
p
tp: lag-time (min)LW: length of longest flow-path (ft)S: slope of the longest flow-path (%)CN: average Curve Numbert: analysis time step
Watershed Lag-Time (L/V)
t5.3,
V60
L3048.06.0maxt
w
wp
tp: watershed lag-time (min)Lw: length of longest flow-path (ft)Vw: longest flow-path average velocity (m/s)t: analysis time step
Watershed Routing
Excess precipitation (mm/hr)
Flow (m3/s)
Time
Pre
cipit
ati
on
Exce
ss
pre
cipi t
ati
on
Flow
Flow = f(Precipitation, Terrain properties, Watershed geomorphology)
Precipitation (mm/hr)
Hydrologic Parameters
Watershed
Abstractions and routing method
Parameters
Stream
Routing method
Parameters
Watershed Parameters
Area
Abtractions:
SCS curve number method (average curve number)
Linear loss rate (initial and constant loss rate)
Routing
SCS curvilinear unit hydrograph (length and slope of longest flow path, average curve number, average velocity in longest flow path)
Hydrologic Parameters
Watershed
Abstractions and routing method
Parameters
Stream
Routing method
Parameters
Routing Method
Flow time (Ls/Vs)
Ls/Vs < t
Muskingum Routing
Ls/Vs > t
Pure Lag Routing
Ls: length of the streamVs: flow velocity in the streamt: analysis time step
Pure-Lag Method
Flow is delayed a fixed amount of time tlag.
)t(I)tt(Q lag
tlag: flow time in the reachI: inflow to the reachQ: outflow from the reach
Pure Lag Parameters
s
slag V60
Lt
tlag: flow time in the reach (min)Ls: reach length (m)Vs: reach average velocity (m/s)
Muskingum Method
Flow is delayed a fixed amount of time K, and redistributed around its centroid.
QIdt
dSandQ)X1(IXKS
S: storage in the reachK: flow time in the reach (t < K < t/2X)X: storage parameterI: inflow to the reachQ: outflow from the reacht: analysis time step
Muskingum Parameters
K: flow time in the reach (hr) [Muskingum K]X: storage parameter [Muskingum X]Ls: reach length (m)Vs: reach average velocity (m/s)n: number of sub-reachest: analysis time step
s
s
V3600
LK
1t
V/L)3/1,X2max(intn ss
Hydrologic Parameters
Watershed
Abstractions and routing method
Parameters
Stream
Routing method
Parameters
Stream Parameters
Length
Routing
Pure lag method (average flow velocity)
Muskingum method (average flow velocity and storage coefficient)