Tropical cyclones (TCs) are one of the largest threats to coastal communities worldwide (Dullaart et al., 2021), and are the costliest natural hazard impacting the United States (Smith & Katz, 2013). Landfalling TCs can bring extreme wind, storm surge, and rainfall to coastal regions, resulting in widespread damage and loss of life. For example, the Galveston hurricane of 1900 caused at least 6,000 fatalities, and remains the deadliest US hurricane to date (Cline, 1900). More recently, Hurricanes Katrina (2005), Sandy (2012), and Harvey (2017) caused extreme flooding due to their rainfall and storm surge with total damages ranging from $80 to $150 billion (2022 USD) for each of the storms (Blake & Zelinsky, 2017;Blake et al., 2013;Knabb et al., 2005). Given the magnitude and frequency of TC-induced catastrophes, it is vital to understand and characterize the wind, rain and surge hazards from historical hurricanes. Developing spatially and temporally continuous records of TC storm characteristics and associated hazards can aid in risk assessment, emergency planning, and mitigation efforts. TC wind, rainfall and surge severity in coastal regions depends on storm characteristics including intensity (maximum sustained wind speed-V max and minimum central pressure-P min ), inner size (i.e., radius to maximum wind-R max ), translation speed, and approach angle to the coast (Irish et al., 2008;Ramos-Valle et al., 2020;Thomas et al., 2019). Peak storm surges also vary based on geographic characteristics, such as coastline shape