Title: Modelling Extreme Events
1 Modelling Extreme Events
2What is an extreme event ?
- Relative to the entity
- House fire
- Florida Windstorm
- Asteroid collision
- Not generally covered by insurance process
- Losses will occur which do have a detrimental
effect on a number of players. These are
generally termed extreme events.
3Overview
- Assessment of Reserves and pricing usually based
on law of large numbers and one distribution - But it should be considered as at least two
- the central part of the distribution, which deals
with the normal claims and - the extreme end of the distribution
4Type of Risks
- Catastrophe Risks
- Mortality Risks
- Asset Value Risks
- Operational Risks
- Other examples at end
5Types of Models
- Statistical/actuarial models, where past
experience is used to estimate the consequence of
future events - Physical models, where, for example, the
consequence of a landslide or submarine
earthquake is estimated from a scaled down model
in a laboratory and - Simulation or catastrophe models depending on
computer simulations of events which include
pre-determined parameters and physical
constraints, for example in weather forecasts.
Catastrophe models tend to make use of
statistical and formulated physical models
6Structure of Models
- Diagnostic, where, for example post event
hurricane loss assessment is made using current
and historic observed data, with, perhaps
physical constraints such as topography, combined
with extrapolating and interpolating the
estimates for known locations to those where
there has been no historic data - Investigative where an explanation is formulated
as to why hurricanes occur and the relationship
between hurricane intensity and, for example,
ocean temperature, and the conditions in the
western Sahara Desert and - Predictive which, for example, attempts to
forecast the number of hurricanes in a season in
certain category or higher.
7Issues in determining model
- Parameter estimation
- How do you estimate 1 in 200 year storm on 25
years data - Outliers are fundamental
- Need to consider range of predictions and not
fixed point - Data
8Generalised Poisson Distribution
- In this talk ignore Frechet. Weibull, Gumbell
- Over some threshold the Generalised Pareto
Distribution (GPD) approximates most
distributions. Therefore to fit the tail of a
distribution (for example, to price a high XL
layer) one needs to select a threshold and then
fit the GPD to the tail - This approach is sometimes known as Peaks over
Threshold or POT. The main issue is the
selection of the threshold, as the distribution
is conditional on that amount.
9Modelling
- Pr(YgtyuYgtu) G(y u, ? , s ) 1 ?y/s
-1/? , for ygt0. - A simple approach is to fit a GPD to a random
variable (say a claim amount) by plotting the
mean exceedance of the random variable,
E(Y-uYgtu) against u. - After some threshold point, the fit will approach
linearity. - Above this point fit a GPD to the data by
calculating ?u Pr(Ygtu) and then using standard
techniques (MLE, Method of Moments) to calculate
? and s.
10Mean Excess Plot Taken from Excel Spreadsheet
11Issues
- At the chosen threshold of 406,000 there are 123
data points - At a threshold of 1,000,000 this reduces to 28.
- At a threshold of 1,500,000 there would be just 7
observations used to fit the GPD. - There is a trade-off between approximation to
the underlying distribution (good for high
threshold) and bias (good for low threshold) - This brutal in the world of extreme values.
12The Power Function
- A Power Law is a function f(x) where the value y
is proportional to some power of the input x - f(x) y x-a
- Power law models tend to relate to geophysical
events. - An example is the Gutenberg-Richter law. Data
indicates that the number of earthquakes of
magnitude M is proportional to 10-bM
13Earthquake Numbers in 1995 and Gutenberg-Richter
Prediction
14Predicted Power Law Exponents for Atmospheric
Phenomena
15The Connection
- Power Laws are related to Pareto Law
- How many people have an income greater than a
specific amount ? - Equivalent in EVT formulation
- How many aggregate claims are greater than a
specific amount ? - The GPD is an extension of Paretos Law
- Self Organising Criticality and Complexity
16Other considerations
- The theorems depend on variables being iid
- There should not be any trend lines, cycles etc
in the data - These need to be removed for the theory to work
17Example Hurricane Data
- Remove trends
- Increase in value of property due to inflation
- Changes of population
- Changes in construction and construction type
- Remove cycles
- Seasonal fluctuations
- El Nino
18Example from modelling storm 90 A
19Hurricane Data from Hogg and Klugman
20Hurricane Data from Hogg and Klugman
21Observations
- Used 5000 (low) threshold
- Highest 1638000(Andrew)- next 863881
22Removing large value
23Observations
- Used 5000 (low) threshold
- Highest 1638000(Andrew)- next 863881
- Adjust Excess to 50000
24Mean Excess at 50000
25PP plot with 50000 threshold
26Parameters
27Observations
- Used 5000 (low) threshold
- Highest 1638000(Andrew)- next 863881
- Adjust Excess to 50000
- Hogg Klugman suggested Lognormal
- GDP gives better fit
- Range of outcomes is calculated
28Range PP Plot
29CDF with 5,000 POT
30CDF with 50,000 POT
31Other Applications
- Operational Loss (Basel II)
- PML for Cargo
- Excess Mortality Bonds
- Terrorism Cover
32Other Applications
- Casulty Excess of Loss
- Patrik found that the right tail of the ISO US
liability claim severity model fitted to claims
generally up to a limit of 1,000,000 is a US
Pareto (or Burr distribution with x-exponent 1)
- The shape parameter of the GPD was approximately
- 1, and that this applied over several lines of
business. - Patrik defined ? -1/a, and estimated the
parameter a.
33Patrik a parameters
PC actuaries should use the GPD to model excess
losses, or make some lame excuse. Extreme
Value Distributions are a necessary part of the
actuarial pricing toolbox, and the parameter -1
is a good initial estimate based on Patriks work.