Ever wondered why a ‘view of risk’ can vary so much between experts, or why your risk assessments based on loss experience don’t match those of catastrophe models?
A good angle to explore these differences from is the Exceedance Probability (EP) curve, a combined view of loss frequency and severity. How these curves are built and what they’re built of varies enormously. As a result, EP curve risk estimations can vary, sometimes, as in this comparative study, by over 100%.
Here we take the example of Japan Typhoon, examining the specific impact of different hazard data sources to highlight what’s going on. We show you hidden aspects of EP curves, clarify why every curve needs some time and attention, and give advice on best practice for storm model validation.
Catastrophe risk assessment and pricing is based either on loss experience and actuarial techniques, or on hazard data that is combined with exposure and vulnerability information in a catastrophe model to generate modelled loss estimates. Exceedance Probability (EP) curves of ‘expected loss’ against ‘return period’ are a common perspective from which to compare the resulting ‘views of risk’.
Knowing how a specific EP curve is built and understanding the variability in the loss experience and hazard data can explain why one ‘view of risk’ is not the same as another. With this knowledge, well informed risk assessment, model validation and pricing decisions can be made.
Multiple ‘views of risk’ can arise for many reasons; in this paper we explore two areas that can lead to differences in Japan Typhoon risk assessment:
1. How a catastrophe model sources and processes hazard data
Wind. For the same past Japan Typhoon events, catastrophe models can select from different tropical cyclone best track data (BTD), leading to notably diverse wind fields in terms of storm intensity and spatial extent (figure 1) and different landfall climatologies, i.e. the annual number of storms making landfall (figure 2). PartnerRe’s in-house tropical cyclone catastrophe model, CatFocus®, shows that parts of the resulting EP curves can vary by over 100% (figure 4).
The BTD selection also impacts EP curves derived from stochastic (model-generated) event sets, as these are based on historic event sets.
Storm surge and flood. A complete typhoon model will also include explicit storm surge and flood components. These aspects are not included in our example as we focus here on the wind component, but they are equally a source of EP curve variations.
2. Availability and treatment of loss experience
EP curves based on typhoon loss experience and actuarial methods also differ depending on the chosen indexation method and loss experience reporting period (figure 4).
The most common hazard data for historical typhoons comes in the form of best track data (BTD), an approximation of an event’s track, size and intensity over time. For Japan Typhoon, two meteorological agencies, JMA and JTWC, provide BTD, each reporting two distinct, but related, intensity metrics, vmax and cpres (see table 1 for definitions).
Figure 1a and b show the extent to which these intensity metrics can differ for a single typhoon event. The availability of the intensity metrics over time is also not consistent (see text box at the end of this article, section “Agency approaches vary”). Our comparative study here uses 1977-2015 historical storms which are covered by the three different intensity metrics JMA vmax, JMA cpres and JTWC vmax; JTWC cpres has only been reported since 2001 and is therefore excluded.
Using BTD track, size and intensity information, catastrophe models employ the physical understanding of typhoons to produce a ‘wind field’ for each storm. Essentially, the model fills in the gaps to give each storm a full associated picture of intensity and movement over time.
Different catastrophe risk experts and vendor modeling companies select one or other or a combination of the three available BTD sources to create their Japan Typhoon wind fields. This BTD choice can have a substantial impact on the resulting wind fields (see figure 1d-f).
A historical typhoon ‘event set’ for Japan comprises all the historical storms that made landfall 2 (hereafter ‘landfalls’), together with their intensity and landfall location data, according to the chosen BTD source. From this, it’s a simple step to compute a ‘landfall climatology’, a summary of the number of Cat 0-5 (i.e. tropical storm and stronger) landfalls per year. Of course, with three possible BTD sources reporting different storm intensities, there are three possible Japan Typhoon landfall climatologies.
As illustrated in figure 2, both the overall number of Cat 0-5 landfalls per year and their Saffir-Simpson Scale intensity categorization can differ substantially depending on the BTD source. For example, in 2013, JTWC vmax results in four Cat 0 landfall events, JMA vmax results in two Cat 0 and two Cat 1 landfall events, and JMA cpres leads to three Cat 0 and two Cat 2 and above landfall events.
Looking at the observed landfall values over time for Japan, figure 2 shows a long-term average of around 3.5 landfalls per year. Variability is also observed on a decadal time-scale, whereby the most recent decade showed about average activity, in contrast to more heightened activity in the 1990s.
Typhoon risk assessment based on loss experience, whereby actuarial methods are applied to the data for direct risk assessment and/or for validation of catastrophe model outputs, requires the loss experience to be complete and homogeneous.
An indication of completeness would be verification against the hazard-based landfall climatology. A perfect match would not be expected, however, due to the risk portfolio’s specific exposure and factors including the extent, location and intensity of the typhoons. However, the differences for Japan Typhoon are particularly notable (figure 3) and rather reflect a change in approach, whereby smaller magnitude events are only included in the more recent loss experience years (2004 to 2015). For the risk assessment of such smaller magnitude events, the loss experience record is therefore only complete for the years 2004-2015.
In terms of homogenization, the loss experience must be re-evaluated for current-day conditions. This process, termed indexation, consists of an adjustment for possible changes in the monetary value of the loss amount (i.e. inflation/deflation), and a normalization in terms of other economic developments in the insurance portfolio, such as changes in the insurance penetration.
Some aspects are more difficult, if not impossible, to homogenize to current-day conditions. These include distinct changes in the geographical concentration of the risk portfolio (e.g. after mergers and acquisitions) or systematic or gradual changes to the underlying policy terms and conditions (e.g. market accepted changes in deductible and limit structures).
To translate hazard data into a measure of loss for the insurance industry, catastrophe models combine the wind fields and landfall climatology data with exposure and vulnerability information. The resulting modeled losses can be expressed as an EP curve, the model’s best estimation of ‘expected loss’ against ‘return period’.
Adopting a single BTD source as the basis of both the wind fields and landfall climatology for each EP curve, and using fixed exposure and vulnerability data, figure 4a shows how each of the three BTD sources for Japan delivers a very different curve. For example, assuming a synthetic, representative portfolio, the estimated 2-year return period loss in figure 4a would be 0.02% of total insured value (TIV) based on JMA vmax, 0.04% of TIV based on JTWC vmax and 0.06% of TIV based on JMA cpres.
The EP curves in figure 4b are based on historical loss experience from the same synthetic portfolio modeled in figure 4a. The number of losses and loss amounts (shown in figure 3) are combined to determine a direct loss-frequency estimation. The observed spread among the (current-day condition) loss-frequency estimations relates to the chosen indexation method (e.g. subject loss, subject premium, inflation, consumer price index or wage index; impact indicated by the length of the vertical bars) and the reporting period. As discussed in the previous section, earlier years in the reported loss experience record often exclude higher frequency, smaller magnitude events. The impact of reporting period is shown by the blue and grey curves; the grey curve uses the full loss experience going back to 1991, whilst the blue curve only uses losses from 2004 (and is therefore not representative of tail events 3). For example, the estimated 2-year return period loss in figure 4b based on the 1991-2015 record is 0.05% of TIV, compared to 0.1% of TIV using the 2004-2015 record. Using only the more recent, and complete, reporting period therefore results in a 100% increase in the estimated loss for 1 to 10-year return period events.
Knowing your EP curves means:
This knowledge enables better judgement of the uncertainties, and therefore determines the level of confidence in a specific ‘view of risk’.
Translating this into best practice for typhoon (and all storm) model validation
When comparing catastrophe model and loss experience based EP curves for the purpose of model validation, we recommend the following key considerations:
Interested in discussing storm model validation for your own portfolio or gaining a greater insight into how we formulate our ‘View of Risk’?
Editor: Dr. Sara Thomas, PartnerRe
Full reference list available on request from the editor: email@example.com
1 Munich Re, NatCatSERVICE, 2014
2 The landfall counts provided in this study also include typhoons that did not make landfall in mainland Japan according to their best track position, but which came within 100 km of the coastline and hence still had the power and reach to cause significant losses from wind, rain and storm surge.
3 Events with a return period of over 10 years
4 Cat Models “Get Real”, PartnerRe (2010)
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