Forecasting Wave Driven Inundation in West Maui – Modelling a Complicated Nearshore Environment to Predict Runup

Martin D. Guiles1, Camilla Tognacchini2, Assaf Azouri3, Volker Roeber4, Ning Li1, Melissa Iwamoto5, Fiona Langenberger5, Tara Owens6 and Douglas S Luther7, (1)University of Hawaii at Manoa, Honolulu, HI, United States, (2)University of Hawaii at Manoa, Oceanography, Honolulu, HI, United States, (3)University of Hawaii, Honolulu, HI, United States, (4)Université de Pau et des Pays de l’Adour, Anglet, France, (5)Pacific Islands Ocean Observing System, Honolulu, United States, (6)University of Hawaii Sea Grant, Wailuku, HI, United States, (7)Univ Hawaii Manoa, Honolulu, HI, United States
Abstract:
Wave-driven runup along the West Maui coastline is producing severe shoreline erosion, damaged infrastructure, and compromised private residences. A better understanding of the phenomena contributing to this runup is needed to enhance both restoration efforts and future resilience of the West Maui coastal region. The complex bathymetric geomorphology in the basin surrounded by Maui, Lānaʻi, Molokaʻi and Kahoʻolawe leads to unique swell shoaling and refraction dynamics. These unique patterns of swell energy have a component that directs significant amplitude into the West Maui coastline for both northern (winter) and southern (summer) swells (the seasonal pattern of swell in Hawaiʻi). The conversion of this pattern of swell energy into the components that drive runup is further complicated by the regions distribution of fringing reef and sloping beaches in the nearshore. Both setup, swash, and infragravity (IG) exhibit significant spatial variability as revealed in runs of the Boussinesq Ocean and Surf Zone (BOSZ) phase resolving model. Comparisons between nearshore pressure sensor data and model runs show excellent skill in modelled nearshore energetics. Extreme cases comprised of maximum values form the last ten years for incoming swell and high sea level give foresite into what could occur now and in the future for this community. Under a NOAA Coastal Resilience award, we have brought together all the necessary pieces to implement a real time two dimensional runup forecast for the community of West Maui. In place we have NOAA Global WAVEWATCH III feeding a high resolution SWAN model which provides directional wave spectra at the offshore boundaries of two large BOSZ model domains. Sea level comes from a new high resolution forecast for Lahaina in the center of the domain. The operational runup forecast has been built and is in the process of threshold validation before its live release on the PacIOOS website.