Mathieu Boudreault’s research while affiliated with Université de Montréal and other places

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Publications (82)


Modelling seasonal mortality: An age–period–cohort approach
  • Preprint
  • File available

May 2025

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138 Reads

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Mathieu Boudreault

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Thomas Landry
Download

Fig. 1. Image generated by Adobe Firefly 2024-11-09.
The profile of experts consulted.
Hierarchy of contributing factors to flood damages according to experts.
Breakdown of home replacement costs and contents.
Comparison of expert contributing factors with literature.

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Flooding: Contributing factors to residential flood damage in Canada

March 2025

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33 Reads

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1 Citation

International Journal of Disaster Risk Reduction


CanMap Address Points over a satellite image in the province of Quebec (Satellite view from Google Maps). The green dots represent residential dwellings, the red dots represent non‐residential usage, and the orange dots indicate mixed‐use properties.
Average TIV according to various rankings of properties.
Map of Canada with provinces highlighted along with the province codes.
Economic Exposure of Canadian Residential Properties to Flooding

February 2025

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50 Reads

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2 Citations

Gabriel Morin

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Mathieu Boudreault

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[...]

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Flood risk management (FRM) involves planning proactively for flooding in high‐risk areas to reduce its impacts on people and property. A key challenge for governments pursuing FRM is to pinpoint assets that are highly economically exposed and vulnerable to flood hazards in order to prioritize them in policy and planning. This paper presents a novel flood risk assessment, making use of a dataset that identifies the location, dwelling type, property characteristics, and potential economic losses of Canadian residential properties. The findings reveal that the average annual costs are $1.4B, but most of the risks are concentrated in high‐risk areas. Data gaps are uncovered that justify replication through local validation studies. The results provide a novel evidence base for specific reforms in Canada's approach to FRM, with a focus on insurance that improves both implementation and effectiveness.


Figure 2: Average number of monthly TCs for the present-day (blue) and the future climate simulation (red) 277 from June to December 278 For each tracked TC, the maximum intensity -defined here as the minimum pressure reached by the cyclone 279 along its trajectory -was determined. Consistent with previous studies ((Hill & Lackmann, 2011; Knutson 280 et al., 2020; Kossin et al., 2020), we found that there are more extreme events in the future climate simulation 281 than in the present-day simulation (Fig. 3) and that the mean storm minimum pressure is deeper in the future 282 climate simulation (-3 hPa). 283 Consistent with other studies (Lee et al., 2020; Studholme et al., 2022), the median TC maximum intensity 284 is slightly shifted northwards of about 1.2° latitude (Fig. 4 a) in a warmer climate because of higher SST that 285 help TCs sustain their intensity at higher latitudes. 286
Figure 9: Box plot of the a) latitude of ET onset for the present-day (blue) and the future climate (red) 361 simulations and b) longitude of ET onset for the present-day (blue) and the future climate simulations (red). 362 The box represents the interquartile range (IQR), containing 50% of the data; the upper edge of the box 363 represents the 75 th percentile (upper quartile -UQ) while the lower edge is the 25 th percentile (lower quartile 364 -LQ). The horizontal line within the box indicates the median, while the green triangle indicates the mean. 365 The whiskers extend to the smallest and largest data points within 1.5 times the IQR from the quartiles. Points 366 beyond the whiskers are considered outliers. 367
Figure 10: Difference in onset ET density between the future climate and the present-day simulations. 374
Figure 11: Box plot of the transition duration (in hours) for the present-day experiment (blue) and the future 391 climate simulations (red) for: a) all storms, and b) storms for which the transition is completed within the 392 regional zone. The box represents the interquartile range (IQR), containing 50% of the data; the upper edge 393 of the box is the 75 th percentile (upper quartile -UQ) while the lower edge is the 25 th percentile (lower quartile 394 -LQ). The horizontal line within the box indicates the median, while the green triangle indicates the mean. 395 The whiskers extend to the smallest and largest data points within 1.5 times the IQR from the quartiles. Points 396 beyond the whiskers are considered outliers. 397
Figure 14: a) Box plot in difference in pressure at the storm center during the transition for the present-day 435 (blue) and the future climate (red) simulations and b) Box plot in relative difference in Integrated Kinetic 436 Energy (for present-day simulations (blue) and future climate simulations (red) during the transition. The box 437 represents the interquartile range (IQR), containing 50% of the data; the upper edge of the box represents the 438 75 th percentile (upper quartile -UQ) while the lower edge is the 25 th percentile (lower quartile -LQ). The 439 horizontal line within the box indicates the median, while the green triangle indicates the mean. The whiskers 440 extend to the smallest and largest data points within 1.5 times the IQR from the quartiles. Points beyond the 441 whiskers are considered outliers. 442
The impacts of climate change on tropical-to-extratropical transitions in the North-Atlantic basin

November 2024

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54 Reads

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1 Citation

As tropical cyclones migrate towards mid-latitudes, they can transform into extratropical cyclones, a process known as extratropical transition. In the North Atlantic basin, nearly half of the hurricanes undergo this transition. After transitioning, these storms can reintensify, posing significant threats to populations and infrastructure along the eastern coast of North America. While the impacts of climate change on hurricanes have been extensively studied, there remain uncertainties about its effects on extratropical transitions. This study aims to assess how climate change affects the frequency, location, intensity, and duration of these transitions. To achieve this, high-resolution regional simulations from an atmospheric regional climate model, based on the RCP 8.5 emissions scenario, were used to compare two 30-year periods: the present (1990–2019) and the end of the century (2071–2100). The results indicate a projected decrease in the number of tropical hurricanes, with no significant change in extratropical transition rates. September and October continue to be the primary months for extratropical transitions. However, the season’s peak appears to have shifted from September to October, suggesting that large-scale environmental conditions may become more favorable for extratropical transitions in October in the future. Although a poleward shift in the maximum intensity of tropical hurricanes is detected, the average latitude of the transitions does not change. Our findings suggest that transitioning storms will be more intense in the future, despite a less baroclinic atmosphere due to a stronger contribution from latent heat transfer. However, the risk of reintensification after transition is not expected to increase.



Flood occurrence and impact models for socioeconomic applications over Canada and the United States

July 2024

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91 Reads

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2 Citations

Large-scale socioeconomic studies of the impacts of floods are difficult and costly for countries such as Canada and the United States due to the large number of rivers and size of watersheds. Such studies are however very important for analyzing spatial patterns and temporal trends to inform large-scale flood risk management decisions and policies. In this paper, we present different flood occurrence and impact models based upon statistical and machine learning methods of over 31 000 watersheds spread across Canada and the US. The models can be quickly calibrated and thereby easily run predictions over thousands of scenarios in a matter of minutes. As applications of the models, we present the geographical distribution of the modelled average annual number of people displaced due to flooding in Canada and the US, as well as various scenario analyses. We find for example that an increase of 10 % in average precipitation yields an increase in the displaced population of 18 % in Canada and 14 % in the US. The model can therefore be used by a broad range of end users ranging from climate scientists to economists who seek to translate climate and socioeconomic scenarios into flood probabilities and impacts measured in terms of the displaced population.


A Global Multi-Source Tropical Cyclone Precipitation (MSTCP) Dataset

June 2024

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151 Reads

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3 Citations

Scientific Data

A global tropical cyclone precipitation dataset covering the period from January 1979 to February 2023 is presented. Global precipitation estimates were taken from the newly developed high-resolution Multi-Source Weighted-Ensemble Precipitation, version 2 (MSWEP V2) and TC tracks were obtained from the International Best Track Archive for Climate Stewardship (IBTrACS) dataset. This Global Multi-Source Tropical Cyclone Precipitation (MSTCP) dataset is comprised of two main products and files in the format of tables: the main and profile datasets. The main file provides various TCP statistics per TC track, including mean and maximum precipitation rates over a fixed and symmetrical radius of 500 km. The profile dataset comprises the azimuthally averaged precipitation every 10-km away from the center of each storm (until 500 km). The case study of Hurricane Harvey is used to show that MSWEP estimates agree well with another commonly used satellite product. The main statistics of the dataset are analyzed as well, including the differences in the dataset metrics for each of the six TC basins and for each Saffir-Simpson category for storm intensity.


Figure 1. Top-down catastrophe modeling approach with climate on top.
Figure 7. Annual simulated pluvial flood probability from 2006 to 2060 over New York, Houston, Chicago and Denver with the GAM model. Similar plots for GLM and RF are available in the SM.
Figure 8. Annual simulated pluvial flooding probability from 2006 to 2060 over Montreal, Toronto and Vancouver with the GAM model. Similar plots for GLM and RF are available in the SM.
Figure 9. Probability density functions of portfolio losses for each portfolio and scenario.
A data science approach to climate change risk assessment applied to pluvial flood occurrences for the United States and Canada

May 2024

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149 Reads

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2 Citations

Astin Bulletin

There is mounting pressure on (re)insurers to quantify the impacts of climate change, notably on the frequency and severity of claims due to weather events such as flooding. This is however a very challenging task for (re)insurers as it requires modeling at the scale of a portfolio and at a high enough spatial resolution to incorporate local climate change effects. In this paper, we introduce a data science approach to climate change risk assessment of pluvial flooding for insurance portfolios over Canada and the United States (US). The underlying flood occurrence model quantifies the financial impacts of short-term (12–48 h) precipitation dynamics over the present (2010–2030) and future climate (2040–2060) by leveraging statistical/machine learning and regional climate models. The flood occurrence model is designed for applications that do not require street-level precision as is often the case for scenario and trend analyses. It is applied at the full scale of Canada and the US over 10–25 km grids. Our analyses show that climate change and urbanization will typically increase losses over Canada and the US, while impacts are strongly heterogeneous from one state or province to another, or even within a territory. Portfolio applications highlight the importance for a (re)insurer to differentiate between future changes in hazard and exposure, as the latter may magnify or attenuate the impacts of climate change on losses.


A Simulation and Empirical Study of the Maximum Likelihood Estimator for Stochastic Volatility Jump-Diffusion Models

March 2024

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18 Reads

Studies in Nonlinear Dynamics and Econometrics

We investigate the behaviour of the maximum likelihood estimator (MLE) for stochastic volatility jump-diffusion models commonly used in financial risk management. A simulation study shows the practical conditions under which the MLE behaves according to theory. In an extensive empirical study based on nine indices and more than 6000 individual stocks, we nonetheless find that the MLE is unable to replicate key higher moments. We then introduce a moment-targeted MLE – robust to model misspecification – and revisit both simulation and empirical studies. We find it performs better than the MLE, improving the management of financial risk.


Projected seasonal flooding in Canada under climate change with statistical and machine learning

March 2024

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85 Reads

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8 Citations

Journal of Hydrology Regional Studies

Study region: Canada Study focus: Floods are among the costliest and deadliest natural hazards in the world. To date, little is known about future seasonal flooding across all Canada. In this paper, data-driven models for flood occurrence (i.e., happening of a flood) and impact (i.e., displaced population) were calibrated for spring and summer seasons in 14,000 watersheds across Canada. Generalized Additive Models (GAM), Random Forests (RF) and Gradient Boosting Machines (GBM) were considered to model seasonal floods. The best-performing flood models were then used with regional climate models to assess the effect of climate change on flooding for three time horizons: historical, medium-term (~2050) and long-term (~2080). New hydrological insights for the region: GAM offered the best out-of-sample performance trade-off in both seasons for predicting flooding in Canada. Projections with GAM showed a general increase in summer flooding occurrence and impact in 2050 and 2080, mainly in the Yukon, western British Columbia, southern Prairies, Ontario and Quebec and some Atlantic provinces. Results for spring flooding were more mixed, but there seemed to be a slight decrease in the impact of spring flooding in the southern Prairies, particularly in 2080. The combination of statistical/machine learning and climate models have provided a more detailed and contrasted picture of the projected seasonal flooding situation over Canada that will help authorities better mitigate future flood risks.


Citations (36)


... The probability of the population exposed to the simulated flood conditions was estimated to quantify the flood loss based on the mortality function method (Li et al. 2023(Li et al. , 2025a. The potential residential economic losses in floods were estimated based on house characteristics and distribution for flood risk assessment (Morin et al. 2025;Shrestha et al. 2024). A quantitative assessment of flood loss probability is of significant importance for the effective management of floods. ...

Reference:

Quantitative estimation of urban flood damage from storm surges for a coastal city
Economic Exposure of Canadian Residential Properties to Flooding

... While successful FRM requires that risk management roles and responsibilities be shared among all private and public actors, the devolution of Canadian water management to local authorities-without an overarching strategy, proper multi-stakeholder and interjurisdictional coordination, and sufficient resources-has created governance challenges (e.g., de Löe & Kreutzwiser, 2007;Saunders & Wenig, 2007;Lyle & McLean, 2008;Henstra et al., 2019a;Morrison et al., 2019;Deschamps et al., 2023). Local governments and Indigenous authorities often struggle to maintain existing infrastructure, possessing limited capacity to invest in costly and complex adaptation measures (Amundsen et al., 2010;Burch, 2010;Thistlethwaite & Henstra, 2017;Oulahen et al., 2018;Fayazi et al., 2020). ...

How Can Municipalities in British Columbia and Quebec Contribute to Flood Risk Reduction?

... Although the model produces wind speeds that align well with historical records, the precipitation rates fromNederhoff et al. (2024) significantly underestimate historical values. To address this underestimation, the model-derived precipitation rates are first standardized then rescaled using values from the Global Multi-Source Tropical Cyclone Precipitation (MSTCP) database(Morin et al., 2024). This adjustment method produces Out-of-sample posterior predictive distribution of damages for the six TCs in the testing set. ...

A Global Multi-Source Tropical Cyclone Precipitation (MSTCP) Dataset

Scientific Data

... GPUs are efficient but a less popular option in practical engineering due to their cost and the high specification of computational hardware required (Fernández-Pato and García-Navarro 2021; Neal et al. 2012). Similarly, ML techniques, such as Artificial Neural Networks, integrate with hydraulic models to speed up processing times; however, the effectiveness of ML models relies on the availability of substantial, event-specific data, which is often lacking, thus limiting their applicability (Grenier et al. 2024;Hosseiny et al. 2023;Mosavi et al. 2018;Schmidt et al. 2020). Simplified hydraulic models speed up calculations by omitting certain terms from the shallow water equations, expediting the computational process significantly compared to more comprehensive 2D models (Ghimire et al. 2014;Horritt and Bates 2002;Hunter et al. 2008;Lin et al. 2005). ...

Projected seasonal flooding in Canada under climate change with statistical and machine learning

Journal of Hydrology Regional Studies

... For simulating the flow of fluids with reference to floods that may occur due to intensification of rainfall or over flooding of rivers the Navier-Stokes equations are used. These equations provide for the dynamics of fluid materials and are basic in analysis of water transport phenomena in rivers, lakes and coastlines [11]. The equations in their incompressible form are:The equations in their incompressible form are: ρ(∂t/∂v+v⋅∇v)=−∇p+μ∇2v+f In this work, the Navier-Stokes equations are used for modeling river flow in an area that is susceptible to flash floods. ...

UQAM‐TCW: A Global Hybrid Tropical Cyclone Wind Model Based Upon Statistical and Coupled Climate Models

... On average, the damage to buildings and property increases with water height (Doyon and Jean 2021;Merz et al. 2010). The curves are constructed either from empirical data from compensation histories or synthetic data based on vulnerability coefficients determined by experts (Aribisala et al. 2022;Deschamps et al. 2023;Romali et al. 2015;Xing et al. 2023). ...

Contributing Factors to Residential Flood Damage in Canada
  • Citing Preprint
  • January 2023

... Instead of being simulation based as with catastrophe models, actuarial models estimate risk based on actual events with loss data. 40 Actuarial models are mostly applied to windstorm 41 and wildfire hazards. [42][43][44][45] Using empirical loss data, the risk can be estimated using econometric methods such as regression. ...

A changing climate for actuarial science
  • Citing Article
  • October 2023

Annals of Actuarial Science

... Managed retreat -the purposeful, coordinated movement of people and assets out of harm's way (Siders, 2019a) -has received increasing attention among academics and practitioners in the fields of climate change adaptation (CCA) and disaster risk reduction (DRR) in recent years (Pinter, 2021;Boudreault et al., 2023). As flood intensities and losses rise (Dottori et al., 2018), and with climate change projections of increasing storm intensity (Seneviratne et al., 2023) and likely sea level rise of up to 1.1 m by 2,100 (Oppenheimer and Glavovic, 2022), there is growing recognition that managed retreat may play an important role in reducing natural hazard risk and adapting to climate change (Kick et al., 2011;Binder et al., OPEN ACCESS EDITED BY 2015; Siders, 2019a;Mach and Siders, 2021;Taylor Aiken and Mabon, 2024). ...

Comparison of three flood-related relocation programs with probabilistic cost-benefit analyses
  • Citing Article
  • August 2023

International Journal of Disaster Risk Reduction

... (Arnell & Gosling, 2013;Döll & Schmied, 2012;Fung et al., 2011). Apart from the impacts of climate change, climate internal variability significantly affects river flow in various regions worldwide (Del Rio Amador et al., 2023;Emerton et al., 2017). The alterations in the sea surface temperature (SST) pattern, specifically the El Niño-Southern Oscillation (ENSO), serve as a prominent indicator of large-scale internal climate variability (Del Rio Amador et al., 2023), exerting substantial influence on the global climate (Del Rio Amador et al., 2023;Ward et al., 2010). ...

Global Asymmetries in the Influence of ENSO on Flood Risk Based on 1,600 Years of Hybrid Simulations

... The DFO database records major floods that can have important socioeconomic consequences and are derived from news, governmental, instrumental, and remote sensing sources. DFO was found to be the most reliable database for this study and was also successfully used in other data-driven flood modelling studies recently (e.g., Grenier et al., 2023;Del Rio Amador et al., 2023;Carozza and Boudreault, 2021;Li et al., 2019a;Liu et al., 2022). ...

Flood Occurrence and Impact Models for Socioeconomic Applications over Canada and the United States
  • Citing Preprint
  • February 2023