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On a risk model with tree-structured Poisson Markov random field frequency, with application to rainfall events

Published online by Cambridge University Press:  23 March 2026

Hélène Cossette
Affiliation:
École d’actuariat, Université Laval , Canada
Benjamin Côté
Affiliation:
University of Waterloo, Canada
Alexandre Dubeau
Affiliation:
École d’actuariat, Université Laval , Canada
Etienne Marceau*
Affiliation:
École d’actuariat, Université Laval , Canada
*
Corresponding author: Etienne Marceau; Email: etienne.marceau@act.ulaval.ca
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Abstract

In many insurance contexts, dependence between risks of a portfolio may arise from their frequencies. We investigate a dependent risk model in which we assume the vector of count variables to be a tree-structured Markov random field with Poisson marginals. The tree structure translates into a wide variety of dependence schemes. We study the global risk of the portfolio and the risk allocation to all its constituents. We provide asymptotic results for portfolios defined on infinitely growing trees. To illustrate its flexibility and computational scalability to higher dimensions, we calibrate the risk model on real-world extreme rainfall data and perform a risk analysis.

Information

Type
Research Article
Creative Commons
Creative Common License - CCCreative Common License - BY
This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (https://creativecommons.org/licenses/by/4.0/), which permits unrestricted re-use, distribution and reproduction, provided the original article is properly cited.
Copyright
© The Author(s), 2026. Published by Cambridge University Press on behalf of The International Actuarial Association
Figure 0

Figure 1. Filial relations in a rooted tree.

Figure 1

Figure 2. Tree $\mathcal{T}$ of Example 2.8 and $\boldsymbol{{N}}$ components’ common shock representations.

Figure 2

Figure 3. Illustration of a Cayley tree and a Bethe lattice, both of degree 3.

Figure 3

Figure 4. Tree structures from Example 4.9.

Figure 4

Figure 5. Cdfs of $S/d$ for Example 4.9.

Figure 5

Table 1. Parameters $\gamma_{\mathcal{W}}$ for each set $\mathcal{W}$ of vertices in Figure 2.

Figure 6

Table 2. Vertex numbers, meteorological stations, and climate ID suffixes, and the datasets in which they are used.

Figure 7

Table 3. Extreme precipitation events threshold u and distribution of cluster sizes (in days) after declustering.

Figure 8

Table 4. Event counts estimates for Datasets 1 and 2.

Figure 9

Table 5. Pairwise Pearson’s correlations for Datasets 1 and 2.

Figure 10

Table 6. Model comparison using BIC and AICc criteria for Datasets 1 and 2.

Figure 11

Table 7. Parameter estimates for the frequency, severity, and dependence structure. Bootstrap standard deviations on 1000 samples are provided for $\boldsymbol{\lambda}$ and $\boldsymbol{\alpha}$.

Figure 12

Figure 6. Correlation-based maximum spanning tree of 10 meteorological stations in Nova Scotia.

Figure 13

Figure 7. Correlation heatmaps of yearly extreme precipitation events counts (left) and amounts (right) comparing empirical (lower triangle) and theoretical (upper triangle).

Figure 14

Table 8. Characteristics and risk measures for $\widetilde{S}$, with comparison to the independent case, $\widetilde{S}^{\perp\!\!\!\perp}$. Values are rounded to the nearest whole number.

Figure 15

Figure 8. Relative contributions to $\text{TVaR}_{\kappa}(Z)$, using the frequency vector $\boldsymbol{{N}} \; (Z = M)$ and the risk model vector $\boldsymbol{{X}} \; (Z = S)$.

Figure 16

Figure 9. $\mathcal{T}$ with vertex sizes scaled based on (a) $C^{\mathrm{Cov}}_{0.99}(X_v, S)$, (b) $C^{\mathrm{TVaR}}_{0.99}(\widetilde{X}_v, \widetilde{S})$, and (c) $\mathbb{E}[X_v]$.

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