An assessment of the spatial distribution of shallow landslides induced by Hurricane Maria in Puerto Rico

Rainfall associated with Hurricane Maria triggered more than 70,000 shallow landslides over a 6,400 km(2)area of Puerto Rico for a mean density of 11.2 slope failures per km(2). When compared to other single storm landslide inventories with similarly sized search areas in tropical and sub-tropical regions, HMA's mean landslide density is eleven times greater than the average. This study relied on frequency and zero-inflated negative binomial regression analyses to explain the spatial variability of landslide densities induced by HMA in relation to soil, geologic terrane, land cover, total storm precipitation, slope, and elevation. Results show that landslide densities tended to be exponentially higher for those areas with the highest rainfall totals and greater on igneous intrusive and other non-limestone sedimentary geologic terranes. Additionally, maximum densities occurred on relatively moderate slopes of 35-50% and not on the steepest hillslopes. Although a resulting regression model over-predicts landslides at lower elevations and underestimates high landslide density areas, it provides an acceptable fit for the landslide densities at a 0.25 km(2)scale. The results presented here can guide future landslide susceptibility analyses to adequately contextualize the heterogeneity of landslide activity caused by extreme tropical cyclones in Puerto Rico and elsewhere.

Automated summary

The study investigates the landslide densities induced by rainfall associated with Hurricane Maria in Puerto Rico. Results show that landslide densities tend to be higher in areas with higher rainfall totals and igneous intrusive and other non-limestone sedimentary geologic terranes. The maximum densities occur on moderate slopes of 35-50%, rather than the steepest hillslopes. The regression model provides an acceptable fit for landslide densities at a 0.25 km(2) scale.