Generalizing the Classical Risk Formula: A Spatial Latent Process Approach

February 28, 2025

Natural hazards continue to pose significant challenges to communities worldwide, making accurate risk assessment models crucial for effective mitigation strategies. Today, I'm excited to share insights from our latest research that aims to revolutionize how we model and understand risk in natural hazard contexts.

Abstract

The classical risk formula expresses damage as a product of asset value and hazard-dependent vulnerability, has served as the foundation of natural hazard risk assessment for decades. While this multiplicative approach has provided valuable insights, the complexity of damage mechanisms suggests the need for a more comprehensive framework. This work introduces a generalized risk formula that incorporates spatial latent processes to capture complex interactions between assets and hazards that the classical multiplication cannot represent. The proposed framework maintains the interpretability of the classical approach while accounting for unobserved spatial dependencies and local vulnerability patterns. The methodology leverages Preconditioned Crank-Nicolson Markov Chain Monte Carlo (pCN MCMC) techniques to efficiently learn the hidden spatial latent processes underlying damage patterns. This generalization addresses a long-standing need in the risk modeling community for capturing spatial interactions and complex damage mechanisms. The framework's flexibility allows for various functional specifications, from simple multiplicative extensions to neural network architectures, providing a unified approach to damage modeling that bridges classical methods with modern statistical learning techniques.

Beyond the Classical Risk Formula

Natural hazard risk assessment traditionally relies on a fundamental conceptual equation that forms the basis of risk quantification:

Risk=Hazard×Exposure×Vulnerability

This core formula serves as the foundation for hazard-specific risk modeling applications across the discipline. The equation presents risk as arising from the interaction of three essential elements, providing a conceptual structure rather than a strict mathematical product. In practice, various interpretations and implementations of this risk framework exist. A notable example is found in the CLIMADA (CLIMate ADAptation) platform, an open-source system widely adopted for climate risk modeling [1], [2]. The CLIMADA formulation expresses risk through the following mathematical structure:

Risk=Probability of Occurrence×DamageDamage=l=1LExposure(sl)f{Hazard(sl)}

The function f() represents vulnerability, sometimes called a fragility or impact function, which estimates the fractional value loss or damage probability for assets subjected to stressors such as wind, flooding, or precipitation [4]. Within this framework, damage constitutes the aggregated monetary impact from asset impairment or destruction at locations s1,s2,,sL, typically reflecting repair or replacement costs. This spatial aggregation reflects standard reporting practices, where damages are typically documented as consolidated totals rather than disaggregated by individual assets.

Limitations of Current Approaches

While this multiplicative relationship has proven invaluable for practical applications, several limitations have become increasingly apparent.

  1. The formula fails to capture complex interactions between exposure and hazard characteristics. The assumption of simple multiplication between asset value and vulnerability is insufficient, as the same wind speed may produce different damage patterns depending on building density, urban layout, or local topography.
  2. The classical formula neglects spatial dependencies by treating each location independently, overlooking crucial spatial correlations in damage patterns. Infrastructure interdependencies, cascading effects, and shared vulnerability characteristics often create spatial patterns that multiplicative models cannot represent.
  3. The approach does not account for hidden factors such as local construction practices, historical development patterns, and socioeconomic factors that can significantly influence vulnerability. These unobserved variables often have spatial structure that affects damage patterns systematically.
  4. The static nature of the classical formula struggles to capture dynamic vulnerability, including underlying vulnerability dynamics, changes during long-lasting disasters, and shifts occurring during compounding disasters and societal shocks [3].

Our Approach: Spatial Latent Process Modeling

Our research introduces a generalized risk formula that integrates spatial latent processes to overcome these limitations. By incorporating a spatially-structured latent variable into the classical framework, we can capture complex, non-linear interactions between exposure and hazard that traditional models miss.

A key innovation in our approach is the application of preconditioned Crank-Nicolson Markov Chain Monte Carlo (pCN MCMC) techniques to learn these spatial latent processes [3]. This efficient algorithm for high-dimensional sampling maintains dimension-independent acceptance rates, making it particularly well-suited for large-scale spatial modeling.

The generalized risk formula can be expressed as:

Damagei=l=1LExposure(sl)f{Hazardi(sl)}X(sl)

where X(sl) represents the spatial latent process that modifies the classic multiplicative relationship, and i indexes the hazard event. This latent process follows a spatial Gaussian process prior [5]:

logX(s)GP(αX,βXR(s,s;θ))

where R(s,s;θ) is a spatial correlation function with parameters θ, and αX and βX control the mean and variance of the process.

Our implementation has revealed important insights about inference challenges in regions with low asset exposure, highlighting a fundamental limitation in risk assessment that has not been previously addressed in the literature.

Recent Related Literature

Recent advances in damage modeling have attempted to address these limitations through various approaches. Machine learning methods have demonstrated success in capturing non-linear relationships between hazard characteristics and damage outcomes [8]. Spatial statistical models have been employed to account for geographic dependencies in vulnerability patterns [6]. Bayesian hierarchical models have shown promise in incorporating uncertainty and learning from multiple events [5], [7].

The integration of physical understanding with data-driven approaches has emerged as a promising direction. Some studies have extended the classical formula through additional terms or modified functional forms [9]. Others have explored the use of latent variable models to capture unobserved risk factors [6], [7]. However, a unified framework that preserves the interpretability of the classical approach while incorporating modern statistical techniques has remained elusive.

Seeking Collaborations

Our research is opening new pathways for improved risk modeling, but many challenges remain. We're actively seeking collaborators in:

  • Domain experts in different natural hazards (hurricanes, floods, wildfires, earthquakes)
  • Insurance and reinsurance industry partners interested in improved risk assessment
  • Climate and environmental scientists working on adaptation and resilience planning

If you're interested in collaboration or have questions about our methodology, please don't hesitate to reach out.

Contact for Collaboration

I look forward to sharing more insights from this research as we continue to develop and refine our approach to generalizing the classical risk formula. Stay tuned for more updates!

References

[1] Aznar-Siguan, G., & Bresch, D. N. (2019). CLIMADA v1: A global weather and climate risk assessment platform. Geoscientific Model Development, 12(7), 3085-3097.

[2] Bresch, D. N., & Aznar-Siguan, G. (2021). CLIMADA v1.4.1: Towards a globally consistent adaptation options appraisal tool. Geoscientific Model Development, 14(1), 351-363.

[3] de Ruiter, M. C., & Van Loon, A. F. (2022). The challenges of dynamic vulnerability and how to assess it. IScience, 25(8).

Cotter, S. L., Roberts, G. O., Stuart, A. M., & White, D. (2013). MCMC methods for functions: Modifying old algorithms to make them faster. Statistical Science, 28(3), 424-446.

Emanuel, K., Sundararajan, R., & Williams, J. (2008). Hurricanes and global warming: Results from downscaling IPCC AR4 simulations. Bulletin of the American Meteorological Society, 89(3), 347-368.

Gelman, A., Simpson, D., & Betancourt, M. (2017). The prior can often only be understood in the context of the likelihood. Entropy, 19(10), 555.

Hu, Z., & Huffer, F. W. (2020). Spatiotemporal analysis of wildfire risk and response in Florida. Natural Hazards, 101, 1-20.

Lallemant, D., Soden, R., Rubinyi, S., Loos, S., Barns, K., & Bhattacharjee, G. (2021). Post-disaster damage assessments as catalysts for recovery: A look at assessments conducted in the wake of the 2015 Gorkha, Nepal, earthquake. Earthquake Spectra, 37(1), 386-404.

Smith, A. B. (2020). 2010-2019: A landmark decade of U.S. billion-dollar weather and climate disasters. NOAA National Centers for Environmental Information.

Woo, G. (2021). Downward counterfactual search for extreme events. Frontiers in Earth Science, 8, 604.