Projected increases in cyclonic storm intensity under a warming climate will have profound effects on forests, potentially changing these ecosystems from carbon sinks to sources. forecasting storm impacts on these ecosystems requires consideration of risk factors associated with storm meteorology, landscape structure, and forest attributes. Here we evaluate risk factors associated with damage severity caused by Hurricanes María and Irma across Puerto Rican forests. Using field and remote sensing data, total forest aboveground biomass (AGB) lost to the storms was estimated at 10.44 (±2.33) Tg, ca. 23% of island-wide pre-hurricane forest AGB. Storm-related rainfall was a stronger predictor of forest damage than maximum wind speeds. Soil water storage capacity was also an important risk factor, corroborating the influence of rainfall on forest damage. Expected increases of 20% in hurricane-associated rainfall in the North Atlantic highlight the need to consider how such shifts, together with high speed winds, will affect terrestrial ecosystems. Cyclonic storms (hurricanes, typhoons, and cyclones) represent the dominant natural disturbance for many coastal forests 1-4. Multiple lines of evidence indicate that atmospheric warming will lead to more intense tropical cyclones 5. Sea surface temperature increases in most regions of tropical cyclone formation suggest that maximum wind speeds will rise and storms are likely to intensify more rapidly 6. Anthropogenic warming will also lead to higher atmosphere moisture content and increases in tropical-cyclone rainfall rates 6-9. Increases in the intensity and frequency of tropical cyclones may reduce the ability of tropical forests to sequester carbon 10. Tropical forests account for ~70% of the gross carbon sink in the world forests (~4.0 Pg C year −1) 11. Although land use change is the predominant driver of change in the tropical forest carbon sink, natural disturbance (e.g., fires, cyclonic storms) can also have important effects 10,12. Models and empirical evidence agree that ecosystems are generally carbon sources immediately following disturbance, but are likely to shift to carbon sinks as vegetation recovers 10,13,14. Forecasting the impacts of a greater number of more severe storms on the ability of tropical forests to act as a carbon sink requires consideration of myriad risk factors that determine the magnitude of storm impacts on vegetation across landscapes. Observational and modelling studies suggest that forests growing at high elevations or on windward slopes are more exposed to high wind speeds, and experience greater damage and tree mortality from severe storms 1,15-18. Associations between topography and tree damage may also be mediated by geology and soil characteristics 19. Restricted root growth of trees growing on ridges, in shallow soils, or soils with poor drainage, may make trees more vulnerable to wind-throw and stem break 1,15,16 , particularly when extreme winds are accompanied by large amounts of rainfall and flooding 20. Forest stand attribute...