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Runoff Calculations Predicting Runoff Depth, Volume and Peak Flow. Environmental Hydrology Lecture 11. Precipitation rate, p (mm/hr). Runoff Production A Refresher. Horton overland flow. Robert E. Horton Image source: American Geophysical Union. p > i overland flow. - PowerPoint PPT Presentation
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Runoff ProductionA Refresher
• Horton overland flow
time
Infil
trat
ion
rate
, i (
mm
/hr)
Pre
cipi
tatio
n r
ate,
p (
mm
/hr)
p > i overland flow
Robert E. HortonImage source:American Geophysical Union
Predicting Runoff and Storm Flow
• The Rational Equation (the SIMPLE model)
– Peak runoff discharge
• The Curve Number concept
– Storm runoff depth runoff volume
• The Graphical Peak Discharge method
– Peak runoff discharge
• Empirical Regression models
– e.g. USGS National Flood Frequency model
The Rational Method
AiCq ***008.1
Where…• q is peak flow in ft3/sec• C in an empirical coefficient• I is the rainfall intensity (in/h)• A is the catchment area (acres)
• The 1.008 factor is… 1 in/h * 1ft/12in *1h/3600sec * 43,560ft2/acre
Concept: Soil Hydrogroups
• Group A: high infiltration (>0.3 in/h), low runoff
• Group B: moderate infiltration when wet (0.15 to 0.30 in/h), moderate runoff
• Group C: slow infiltration when wet (0.05 to 0.15 in/h), high runoff
• Group D: very low infiltration when wet (<0.05 in/h), very high runoff
Rational Method Assumptions and Limitations
• Rainfall is uniform
• Time of concentration (tc) is the time required for water to get from the most distant point in the watershed to the point of observation
• Peak runoff ≈ Peak rainfall intensity lagged by tc
• Frequency of runoff ≈ frequency of rainfall
• Best for small watersheds (<1 mile2)
Derivation of the CN equation
QFIP a
S
F
IP
Q
a
)(
SIa
Where…
P = precipitation (in)
Ia = initial abstraction (in)
F = cumulative infiltration (in)
Q = direct runoff (in)S = max. potential retention (in)
λ = coefficient, usually 0.2
)(
)( 2
SIP
IPQ
a
a
)8.0(
)2.0( 2
SP
SPQ
Mass Balance
Proportionality
SubstitutionS=f(P-Ia, Q)
Proportionality
Substitution
CN = curve number
inchesfor 101000
CN
S
mmfor 25425400
CN
STR-55 Manual, see also Mishra et al. 2006
Concept: Antecedent Moisture Content(based on previous 5-day P)
• AMC-1 (Dry)– Dormant season P <0.5 in– Growing Season P <1.4 in
• AMC-2 (Average)– Dormant season 0.5<P <1.1 in– Growing Season 1.4<P <2.1 in
• AMC-3 (Wet)– Dormant season P >1.1 in– Growing Season P >2.1 in
Curve Number Adjustments for AMC
Ward and Trimble, after NRCS
0.0
0.5
1.0
1.5
2.0
2.5
0 20 40 60 80 100
CN forAMC-II
Adj
ustm
ent F
act
or
AMC-III
AMC-II
AMC-I
Curve Number (TR-55)Assumptions and Limitations
• Describes average and not extreme events
• Does not explicitly account for storm duration or intensity
• The term Ia is ill-defined and has important influences on the derivation of CN’s
• Does not deal with snow or rain on frozen ground
• Should not be used for storms <0.5 in
• Does not explicitly deal with groundwater effects
• Don’t use if the weighted CN is <40, inaccurate
The Graphical Peak Discharge Method
Where…• q is the peak runoff (ft3/sec)
• qu is the unit peak discharge (ft3/sec per square mile per inch of rain or csm/in)
• A is area (square miles)• Q is the total runoff depth (from CN, in inches)• F is a ponding adjustment factor
FQAqq u ***
Can be used to relate Q from CN approach to q.Essentially relates storm volume to storm peak q.
The Graphical MethodAssumptions and Limitations
• Homogenous land cover/use in catchment
• Only one main stream, or an balance network
• “ponding” is off-stream, not in-stream
• Need some idea of Ia
• Need tc = f(hydraulic length, maximum retention [S], land slope, return interval)
Empirical Regression Models
• Where• DA = drainage area• S = channel bed slope• P = reference precipitation (e.g. 2y/24h)• BDF = an index of development• IC = percent impervious cover• U = indices of other land uses• STR = percent lakes, ponds, wetlands• E = elevation effect• Qft = the reference discharge event (e.g. 2y/24h)• X, a, b, c,… are fitted coefficients
ift
ihgf
edcbRI
QESTRUIC
BDFXPSDAaq
)()()1()()(
)13()()()(
This equation is used by FEMA for national flood forecasting (See NFF model)