Bivariate Flood Frequency Analysis using Copula with Parametric and Nonparametric Marginals

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Bivariate Flood Frequency Analysis using Copula with Parametric and Nonparametric Marginals. Subhankar Karmakar Slobodan P. Simonovic The University of Western Ontario The Institute for Catastrophic Loss Reduction. Presentation outline. Introduction Objectives of the study Study area - PowerPoint PPT Presentation

Transcript of Bivariate Flood Frequency Analysis using Copula with Parametric and Nonparametric Marginals

Bivariate Flood Frequency Analysis using Copula with

Parametric and Nonparametric Marginals

Subhankar KarmakarSlobodan P. Simonovic

The University of Western OntarioThe Institute for Catastrophic Loss

Reduction

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Presentation outline

Introduction Objectives of the study Study area

Data and flood characteristics Marginal distributions of flood

characteristics Parametric and nonparametric estimation

Joint and conditional distributions using copula

Conclusions

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Introduction

Flood management (design, planning, operations) requires knowledge of flood event characteristics

Flood characteristics

Peak flow DurationVolume

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Introduction

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Introduction

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Study objectives To determine appropriate marginal distributions

for peak flow, volume and duration using parametric and nonparametric approaches

To define marginal distribution using orthonormal series method

To apply the concept of copulas by selecting marginals from different families of probability density functions

To establish joint and conditional distributions of different combinations of flood characteristics and corresponding return periods

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Study area Red River Basin 116,500 km2 (89% in

USA 11% in CDN) Flooding in the basin

is natural phenomena

Historical floods: 1826; 1950; 1997

Size of the basin and flow direction

No single solution to the flood mitigation challenge

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Study area - data

Daily streamflow data for 70 years (1936-2005)

Gauging station (05082500) - Grand Forks, North Dakota, US Location - latitude 47°55'37"N and longitude

97°01'44"W Drainage area - 30,100 square miles Contributing area - 26,300 square miles

http://waterdata.usgs.gov

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Study area – flood characteristics

Dependence between P, V and D

P and V highly correlated All the correlations positive

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Marginals - parametric

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Marginals - nonparametric

Nonparametric kernel estimation of flood frequency

Orthonormal series method

n

1ll

1 }h/)xx{(K)nh()x(f̂

js0dx)x()x( js j1dx)}x({ 2j

1)x(0 )jxcos(2)x(j

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Results

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Results

P follows gamma distribution (parametric) and V and D follow distribution function obtained

from orthonormal series method (nonparametric)

Mixed marginals

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Results

Second test

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Copula

An alternative way of modeling the correlation structure between random variables.

They dissociate the correlation structure from the marginal distributions of the individual variables.

n - dimensional distribution function can be written: ))x(F),......,x(F(C)x,......,x(F nn11n1

1,.....,0)),(),......,((),......,( 11

11

11 nnnn uuuFuFFuuC

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Copula

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Results – joint distributions

Peak flow - Volume

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Results – joint distributions

Volume - Duration

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Results – joint distributions

Peak flow - Duration

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Results – conditional distributions

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Results – conditional distributions

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Results – conditional distributions

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Results – return period

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Conclusions Concept of copula is used for evaluating joint

distribution function with mixed marginal distributions - eliminates the restriction of selecting marginals for flood variables from the same family of probability density functions.

Nonparametric methods (kernel density estimation and orthonormal series) are used to determine the distribution functions for peak flow, volume and duration.

Nonparametric method based on orthonormal series is more appropriate than kernel estimation.