Modelling and Estimating the Clustering of Extreme Events Rob Lamb 3 - - PowerPoint PPT Presentation

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Modelling and Estimating the Clustering of Extreme Events Rob Lamb 3 - - PowerPoint PPT Presentation

Modelling and Estimating the Clustering of Extreme Events Rob Lamb 3 , 4 Ross Towe 1 Jonathan Tawn 2 1 School of Computing and Communications, Lancaster University, Lancaster, UK 2 Department of Mathematics and Statistics, Lancaster University,


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SLIDE 1

Modelling and Estimating the Clustering of Extreme Events

Ross Towe 1 Jonathan Tawn 2 Rob Lamb 3,4

1School of Computing and Communications, Lancaster University, Lancaster, UK 2Department of Mathematics and Statistics, Lancaster University, Lancaster, UK 3JBA Trust, Broughton Hall, Skipton, UK 4Lancaster Environment Centre, Lancaster University, Lancaster, UK

September 2017

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SLIDE 2

Motivation

Credit: BBC NEWS Credit: Barry Hankin, JBA Consulting

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SLIDE 3

Motivation

  • Regular occurrences of multiple extreme events being
  • bserved in the same season
  • Large events are wrongly assumed to be independent and

identically distributed

  • Clustering of apparently independent exists due to local

non-stationarity

  • Develop a risk measure to characterise the heightened local

risk of extreme events

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SLIDE 4

Stage Data

Nov Jan 0.2 0.4 0.6 0.8 1.0 Date Stage

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SLIDE 5

Stage Data

Nov Jan 0.2 0.4 0.6 0.8 1.0 Date Stage

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SLIDE 6

Modelling Strategy

2000 2005 2010 0.0 0.2 0.4 0.6 0.8 1.0 1.2 1.4 Date Stage

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SLIDE 7

Poisson Process

  • Consider set of IID exceedances Z1, . . . , Zn above a

sufficiently high threshold u

  • Number of points N above the threshold u:

N ∼ Poisson(Λ(z, u))

  • Characterise the exceedances in terms of the following

parameters:

  • Location parameter µ ∈ R
  • Scale parameter σ ≥ 0
  • Shape parameter ξ ∈ R

G(z) = exp {−Λ(z, u)} = exp

  • 1 + ξ

z − µ σ −1/ξ

+

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SLIDE 8

Poisson Process

Covariate Effects

Z ∼ PP(µ(x) = 20 + 2x, σ = 2, ξ = 0.1), where x ∼ N(0, 1)

  • 1

2 3 4 5 16 18 20 22 24 Time Observations

  • x=0.77

x=0.06 x=−0.74 x=−0.49 x=−2.26

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SLIDE 9

Definition of Relative Risk

Relative Risk Definition R > 1 An event of at least size z is R times more likely to occur if a 1 in T year event was already observed. R = 1 There is no change in the risk of an event

  • f at least size z occurring even if a 1 in T

year event has already been observed. R < 1 An event of at least size z is R times less likely to occur if a 1 in T year event was already observed.

Table: Definition of Relative Risk

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SLIDE 10

Relative Risk Measure

  • Time

t 1

u ZT ZS

  • A

Relative Risk = P(M⌊tn⌋+1:n > zS|M1:⌊tn⌋ = zT) P(M1:n > zS)

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SLIDE 11

Simulated Example

1 in 100 year event and t=0.4

Z ∼ PP(µ(x) = 20 + 2x, σ = 2, ξ = ±0.1), where x ∼ N(0, 1)

1 5 10 50 500 2 4 6 8 10 12 Return Period Relative Risk

Positive ξ

1 5 10 50 500 2 4 6 8 10 12 Return Period Relative Risk

Negative ξ

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SLIDE 12

Case Study

  • Three hourly measurements of

Stage from the River Harbourne from 1998−2012

  • Focus of many studies by the

Environment Agency

  • Harbertonford has been flooded 21

times in the past 60 years

  • Was flooded 6 times between 1998

and 2000

Credit: Environment Agency

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SLIDE 13

Covariate Relationship

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SLIDE 14

Covariate Relationship

Complexity:

  • Difficult to detect large scale effects at a single location
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SLIDE 15

Covariate Relationship

Complexity:

  • Difficult to detect large scale effects at a single location
  • Nearby rainfall gauges fail to explain changes in extremal

behaviour

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SLIDE 16

Covariate Relationship

Solution:

  • Estimate the parameters using a Bayesian framework
  • MCMC with a Metropolis Hastings algorithm
  • Introduce a random effect in the location parameter

Gz|s(z) = exp

  • 1 + ξ

z − µ(s) σ −1/ξ

+

  • ,

where µ(s) = µ0 + µ1si and si ∼ N(0, 1)

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SLIDE 17

Random Effect Estimates

Estimates of si

  • 2000

2005 2010 −3 −2 −1 1 2 Year Estimate

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SLIDE 18

Relative Risk Estimate for Harbertonford

Extreme Event in October

1 5 10 50 500 2 4 6 8 10 12 Return Period Relative Risk

10 year 100 year 1000 year 10 year 100 year 1000 year

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SLIDE 19

Relative Risk Estimate for Harbertonford

Extreme Event in January

1 5 10 50 500 2 4 6 8 10 12 Return Period Relative Risk

10 year 100 year 1000 year

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SLIDE 20

Conclusion and Further Work

  • Development of risk measures which conveys the change in

risk once extreme events have been observed

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SLIDE 21

Conclusion and Further Work

  • Development of risk measures which conveys the change in

risk once extreme events have been observed

  • Illustration of methodology to a south Devon catchment
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SLIDE 22

Conclusion and Further Work

  • Development of risk measures which conveys the change in

risk once extreme events have been observed

  • Illustration of methodology to a south Devon catchment
  • Extension to consider unobserved covariates
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SLIDE 23

Conclusion and Further Work

  • Development of risk measures which conveys the change in

risk once extreme events have been observed

  • Illustration of methodology to a south Devon catchment
  • Extension to consider unobserved covariates
  • Consider more complex covariate relationships
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SLIDE 24

Conclusion and Further Work

  • Development of risk measures which conveys the change in

risk once extreme events have been observed

  • Illustration of methodology to a south Devon catchment
  • Extension to consider unobserved covariates
  • Consider more complex covariate relationships
  • Consider alternative risk measures
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SLIDE 25

Conclusion and Further Work

  • Development of risk measures which conveys the change in

risk once extreme events have been observed

  • Illustration of methodology to a south Devon catchment
  • Extension to consider unobserved covariates
  • Consider more complex covariate relationships
  • Consider alternative risk measures

Any questions?

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SLIDE 26

Second Risk Measure

  • Time

t 1

u ZT

  • A

Relative Risk 2 = P(M⌊tn⌋+1:n > zT|N1:⌊tn⌋ = n1) P(M1:n > zT)

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SLIDE 27

Second Risk Measure

Simulated example

Positive ξ Negative ξ

2 5 10 20 50 100 500 1 2 3 4 New T year event Relative Risk