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          Title: 
            NEOWAVE Regional Tsunami Model: Kalapana 1975: Hawaii: Maui
          Date: 
            Date: 
              Date: 
                Date: 
                  2022-05-06
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            Related publication: Yamazaki, Y., Kowalik, Z. and Cheung, K.F. 
            (2009), Depth-integrated, non-hydrostatic model for wave breaking 
            and run-up. Int. J. Numer. Meth. Fluids, 61: 473-497. 
            https://doi.org/10.1002/fld.1952.
      Abstract: 
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        hazard map of wave amplitude based on the 1975 Kalapana tsunami. Data 
        are gridded at approximately 180-m resolution referenced to the WGS84 
        coordinate system and use a vertical datum of mean sea level (MSL). 
        This shock-capturing, dispersive wave model computes tsunami 
        generation, propagation, and inundation for complex flow patterns in 
        shelf and reef environments. It has been validated with analytical, 
        laboratory, and field benchmarks and is approved by the National 
        Tsunami Hazard Mitigation Program. These hazard maps cover tsunamis 
        only; other potential hazards such as wind waves and swells would be 
        additive to the inundation described by these data.
      Purpose: 
        PacIOOS provides timely, reliable, and accurate ocean information to 
        support a safe, clean, productive ocean and resilient coastal zone in 
        the U.S. Pacific Islands region.
      Credit: 
        The Pacific Islands Ocean Observing System (PacIOOS) is funded through 
        the National Oceanic and Atmospheric Administration (NOAA) as a 
        Regional Association within the U.S. Integrated Ocean Observing System 
        (IOOS). PacIOOS is coordinated by the University of Hawaii School of 
        Ocean and Earth Science and Technology (SOEST).
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            The data may be used and redistributed for free but is not 
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            the data Contributor, University of Hawaii, PacIOOS, NOAA, State 
            of Hawaii nor the United States Government, nor any of their 
            employees or contractors, makes any warranty, express or implied, 
            including warranties of merchantability and fitness for a 
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        hazard map of wave amplitude based on the 1975 Kalapana tsunami. Data 
        are gridded at approximately 180-m resolution referenced to the WGS84 
        coordinate system and use a vertical datum of mean sea level (MSL). 
        This shock-capturing, dispersive wave model computes tsunami 
        generation, propagation, and inundation for complex flow patterns in 
        shelf and reef environments. It has been validated with analytical, 
        laboratory, and field benchmarks and is approved by the National 
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        hazard map of wave amplitude based on the 1975 Kalapana tsunami. Data 
        are gridded at approximately 180-m resolution referenced to the WGS84 
        coordinate system and use a vertical datum of mean sea level (MSL). 
        This shock-capturing, dispersive wave model computes tsunami 
        generation, propagation, and inundation for complex flow patterns in 
        shelf and reef environments. It has been validated with analytical, 
        laboratory, and field benchmarks and is approved by the National 
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        hazard map of wave amplitude based on the 1975 Kalapana tsunami. Data 
        are gridded at approximately 180-m resolution referenced to the WGS84 
        coordinate system and use a vertical datum of mean sea level (MSL). 
        This shock-capturing, dispersive wave model computes tsunami 
        generation, propagation, and inundation for complex flow patterns in 
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