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          Title: 
            Tsunami Run-Up Inundation With 0.5-m Sea Level Rise: Honolulu, 
            Hawaii
          Date: 
            Date: 
              Date: 
                Date: 
                  2014-09-26
              Date_Type: 
                Date_Type_Code: 
                  creation
          Date: 
            Date: 
              Date: 
                Date: 
                  2014-09-26
              Date_Type: 
                Date_Type_Code: 
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              Date: 
                Date: 
                  2014-09-26
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              Individual_Name: 
                Kwok Fai Cheung
              Organisation_Name: 
                University of Hawaii at Manoa
              Contact_Information: 
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                    Address: 
                      Electronic_Mail_Address: 
                        cheung@hawaii.edu
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      Abstract: 
        Computer model simulation of tsunami run-up inundation around 
        Honolulu, Hawaii including half a meter of sea level rise at mean 
        higher high water (MHHW) as its baseline water level. The study area 
        includes the urban corridor stretching from Pearl Harbor to Waikiki 
        and Diamond Head along the south shore of the island of Oahu. The 
        model simulates maximum inundation based on five major historical 
        tsunamis that have impacted Hawaii: 1) The 1946 Aleutian earthquake 
        (8.2 Mw), 2) 1952 Kamchatka earthquake (9.0 Mw), 3) 1957 Aleutian 
        earthquake (8.6 Mw), 4) 1960 Chile earthquake (9.5 Mw), and 5) the 
        1964 Alaska earthquake (9.2 Mw).
        
        Model results produced in 2014 by Dr. Kwok Fai Cheung of the 
        department of Ocean and Resources Engineering (ORE) in the School of 
        Ocean and Earth Science and Technology (SOEST) of the University of 
        Hawaii at Manoa. Supported in part by the NOAA Coastal Storms Program 
        (CSP) and the University of Hawaii Sea Grant College Program. While 
        considerable effort has been made to implement all model components in 
        a thorough, correct, and accurate manner, numerous sources of error 
        are possible. These data do not consider future changes in coastal 
        geomorphology and natural processes such as erosion, subsidence, or 
        future construction. These data do not specify timing of inundation 
        depths and are not appropriate for conducting detailed spatial 
        analysis. The entire risk associated with the results and performance 
        of these data is assumed by the user. These data should be used 
        strictly as a planning reference and not for navigation, permitting, 
        or other legal purposes.
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        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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          Keyword: 
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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, 
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            particular purpose, or assumes any legal liability for the 
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            Tsunami Run-Up Inundation With 0.5-m Sea Level Rise: Honolulu, 
            Hawaii
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              Date: 
                Date: 
                  2014-09-26
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        higher high water (MHHW) as its baseline water level. The study area 
        includes the urban corridor stretching from Pearl Harbor to Waikiki 
        and Diamond Head along the south shore of the island of Oahu. The 
        model simulates maximum inundation based on five major historical 
        tsunamis that have impacted Hawaii: 1) The 1946 Aleutian earthquake 
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        earthquake (8.6 Mw), 4) 1960 Chile earthquake (9.5 Mw), and 5) the 
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        Model results produced in 2014 by Dr. Kwok Fai Cheung of the 
        department of Ocean and Resources Engineering (ORE) in the School of 
        Ocean and Earth Science and Technology (SOEST) of the University of 
        Hawaii at Manoa. Supported in part by the NOAA Coastal Storms Program 
        (CSP) and the University of Hawaii Sea Grant College Program. While 
        considerable effort has been made to implement all model components in 
        a thorough, correct, and accurate manner, numerous sources of error 
        are possible. These data do not consider future changes in coastal 
        geomorphology and natural processes such as erosion, subsidence, or 
        future construction. These data do not specify timing of inundation 
        depths and are not appropriate for conducting detailed spatial 
        analysis. The entire risk associated with the results and performance 
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            Hawaii
          Date: 
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              Date: 
                Date: 
                  2014-09-26
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      Abstract: 
        Computer model simulation of tsunami run-up inundation around 
        Honolulu, Hawaii including half a meter of sea level rise at mean 
        higher high water (MHHW) as its baseline water level. The study area 
        includes the urban corridor stretching from Pearl Harbor to Waikiki 
        and Diamond Head along the south shore of the island of Oahu. The 
        model simulates maximum inundation based on five major historical 
        tsunamis that have impacted Hawaii: 1) The 1946 Aleutian earthquake 
        (8.2 Mw), 2) 1952 Kamchatka earthquake (9.0 Mw), 3) 1957 Aleutian 
        earthquake (8.6 Mw), 4) 1960 Chile earthquake (9.5 Mw), and 5) the 
        1964 Alaska earthquake (9.2 Mw).
        
        Model results produced in 2014 by Dr. Kwok Fai Cheung of the 
        department of Ocean and Resources Engineering (ORE) in the School of 
        Ocean and Earth Science and Technology (SOEST) of the University of 
        Hawaii at Manoa. Supported in part by the NOAA Coastal Storms Program 
        (CSP) and the University of Hawaii Sea Grant College Program. While 
        considerable effort has been made to implement all model components in 
        a thorough, correct, and accurate manner, numerous sources of error 
        are possible. These data do not consider future changes in coastal 
        geomorphology and natural processes such as erosion, subsidence, or 
        future construction. These data do not specify timing of inundation 
        depths and are not appropriate for conducting detailed spatial 
        analysis. The entire risk associated with the results and performance 
        of these data is assumed by the user. These data should be used 
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            Hawaii
          Date: 
            Date: 
              Date: 
                Date: 
                  2014-09-26
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      Abstract: 
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        Honolulu, Hawaii including half a meter of sea level rise at mean 
        higher high water (MHHW) as its baseline water level. The study area 
        includes the urban corridor stretching from Pearl Harbor to Waikiki 
        and Diamond Head along the south shore of the island of Oahu. The 
        model simulates maximum inundation based on five major historical 
        tsunamis that have impacted Hawaii: 1) The 1946 Aleutian earthquake 
        (8.2 Mw), 2) 1952 Kamchatka earthquake (9.0 Mw), 3) 1957 Aleutian 
        earthquake (8.6 Mw), 4) 1960 Chile earthquake (9.5 Mw), and 5) the 
        1964 Alaska earthquake (9.2 Mw).
        
        Model results produced in 2014 by Dr. Kwok Fai Cheung of the 
        department of Ocean and Resources Engineering (ORE) in the School of 
        Ocean and Earth Science and Technology (SOEST) of the University of 
        Hawaii at Manoa. Supported in part by the NOAA Coastal Storms Program 
        (CSP) and the University of Hawaii Sea Grant College Program. While 
        considerable effort has been made to implement all model components in 
        a thorough, correct, and accurate manner, numerous sources of error 
        are possible. These data do not consider future changes in coastal 
        geomorphology and natural processes such as erosion, subsidence, or 
        future construction. These data do not specify timing of inundation 
        depths and are not appropriate for conducting detailed spatial 
        analysis. The entire risk associated with the results and performance 
        of these data is assumed by the user. These data should be used 
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        or other legal purposes.
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                  Linkage: 
                    URL: 
                      http://geo.pacioos.hawaii.edu/geoserver/
                  Protocol: 
                    http
                  Name: 
                    GeoServer
                  Description: 
                    This URL provides access to this dataset via GeoServer, 
                    including multiple output formats and an OpenLayers viewer.
                  Function: 
                    OnLine_Function_Code: 
                      download
          Distributor_Transfer_Options: 
            Digital_Transfer_Options: 
              Online: 
                Online_Resource: 
                  Linkage: 
                    URL: 
                      http://geo.pacioos.hawaii.edu/geoexplorer/
                  Protocol: 
                    http
                  Name: 
                    GeoExplorer
                  Description: 
                    This URL provides a viewer for this dataset.
                  Function: 
                    OnLine_Function_Code: 
                      download
  Data_Quality_Information: 
    Data_Quality: 
      Scope: 
        Scope: 
          Hierarchy_Level: 
            Scope_Code: 
              dataset
      Lineage: 
        Lineage: 
          Statement: 
            2014-09-26T00:00:00Z OGC web services (WMS and WFS) enabled by 
            PacIOOS via GeoServer. Original data from source provider may have 
            been reformatted, reprojected, or adjusted in other ways to 
            optimize these capabilities.
  Metadata_Maintenance: 
    Maintenance_Information: 
      Maintenance_And_Update_Frequency: 
      Maintenance_Note: 
        This record was translated and enhanced from GeoServer OGC Web 
        Services (OWS) using PacIOOS software.