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Dataset Title: | NEOWAVE Regional Tsunami Model: Guam: Merizo |
Institution: | Pacific Islands Ocean Observing System (PacIOOS) (Dataset ID: neowave_merizo) |
Information: | Summary | License | FGDC | ISO 19115 | Metadata | Background | Data Access Form |
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Attributes { latitude { String _CoordinateAxisType "Lat"; Float32 actual_range 13.22, 13.32; String axis "Y"; String ioos_category "Location"; String long_name "Latitude"; String short_name "lat"; String standard_name "latitude"; String units "degrees_north"; } longitude { String _CoordinateAxisType "Lon"; Float32 actual_range 144.63, 144.7125; String axis "X"; String ioos_category "Location"; String long_name "Longitude"; String short_name "lon"; String standard_name "longitude"; String units "degrees_east"; } ssh_local_preferred { Float32 _FillValue -9999.0; Float64 colorBarMaximum 9.0; Float64 colorBarMinimum 0.0; String comment "Inundation, or maximum sea surface elevation over the flooded area; vertical datum is mean sea level. Based on an Mw 8.3 Mariana Trench earthquake, which is the preferred maximum from the Global Earthquake Model. The term \"preferred maximum\" is commonly used in the seismological community for the largest earthquake expected at a subduction zone and used for evacuation of coastal residents during a tsunami."; String ioos_category "Sea Level"; String long_name "sea surface height for preferred maximum local event"; Float32 missing_value -9999.0; String short_name "ssh"; String standard_name "sea_surface_height"; String units "meters"; Float32 valid_range 0.0, 10.0; } ssh_local_considered { Float32 _FillValue -9999.0; Float64 colorBarMaximum 9.0; Float64 colorBarMinimum 0.0; String comment "Inundation, or maximum sea surface elevation over the flooded area; vertical datum is mean sea level. Based on a maximum considered Mw 8.5 Mariana Trench earthquake, which is Mw 0.2 higher than the preferred maximum from the Global Earthquake Model. The term \"maximum considered\" is commonly used by engineers for the largest earthquake used in the design of buildings and infrastructure and for the siting of tsunami evacuation shelters."; String ioos_category "Sea Level"; String long_name "sea surface height for maximum considered local event"; Float32 missing_value -9999.0; String short_name "ssh"; String standard_name "sea_surface_height"; String units "meters"; } ssh_distant_preferred { Float32 _FillValue -9999.0; Float64 colorBarMaximum 6.0; Float64 colorBarMinimum 0.0; String comment "Inundation, or maximum sea surface elevation over the flooded area; vertical datum is mean sea level. Based on aggregations (envelopes) of tsunamis generated by the preferred maximum Mw 9.3 Kuril, 8.7 Nankai, 8.5 Philippine, and 8.8 New Guinea earthquakes from the Global Earthquake Model. The term \"preferred maximum\" is commonly used in the seismological community for the largest earthquake expected at a subduction zone and used for evacuation of coastal residents during a tsunami."; String ioos_category "Sea Level"; String long_name "sea surface height for preferred maximum distant event"; Float32 missing_value -9999.0; String short_name "ssh"; String standard_name "sea_surface_height"; String units "meters"; } ssh_distant_considered { Float32 _FillValue -9999.0; Float64 colorBarMaximum 6.0; Float64 colorBarMinimum 0.0; String comment "Inundation, or maximum sea surface elevation over the flooded area; vertical datum is mean sea level. Based on aggregations (envelopes) of tsunamis generated by the maximum considered Mw 9.5 Kuril, 8.9 Nankai, 8.7 Philippine, and 9.0 New Guinea earthquakes, which are Mw 0.2 higher than the preferred maximum from the Global Earthquake Model. The term \"maximum considered\" is commonly used by engineers for the largest earthquake used in the design of buildings and infrastructure and for the siting of tsunami evacuation shelters."; String ioos_category "Sea Level"; String long_name "sea surface height for maximum considered distant event"; Float32 missing_value -9999.0; String short_name "ssh"; String standard_name "sea_surface_height"; String units "meters"; } NC_GLOBAL { String acknowledgement "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)."; String cdm_data_type "Grid"; String comment "Model runs produced by Kwok Fai Cheung (cheung@hawaii.edu)."; String Conventions "CF-1.6, ACDD-1.3"; String creator_email "cheung@hawaii.edu"; String creator_institution "University of Hawaii at Manoa"; String creator_name "Kwok Fai Cheung"; String creator_type "person"; String creator_url "https://www.soest.hawaii.edu/ore/people/faculty/kwok-fai-cheung/"; String date_created "2022-09-08"; String date_issued "2022-09-08"; String date_metadata_modified "2022-09-08"; String date_modified "2022-09-08"; String defaultGraphQuery "ssh_local_preferred"; String drawLandMask "off"; Float64 Easternmost_Easting 144.7125; String geospatial_bounds "POLYGON ((13.2200 144.6300, 13.3200 144.6300, 13.3200 144.7125, 13.2200 144.7125, 13.2200 144.6300))"; String geospatial_bounds_crs "EPSG:4326"; Float64 geospatial_lat_max 13.32; Float64 geospatial_lat_min 13.22; String geospatial_lat_units "degrees_north"; Float64 geospatial_lon_max 144.7125; Float64 geospatial_lon_min 144.63; String geospatial_lon_units "degrees_east"; String history "2022-09-08T21:00:00Z New dataset. 2024-10-06T05:02:19Z https://pae-paha.pacioos.hawaii.edu/thredds/dodsC/neowave_merizo 2024-10-06T05:02:19Z https://pae-paha.pacioos.hawaii.edu/griddap/neowave_merizo.das"; String id "neowave_merizo"; String infoUrl "https://www.soest.hawaii.edu/ore/people/faculty/kwok-fai-cheung/"; String institution "Pacific Islands Ocean Observing System (PacIOOS)"; String instrument "Not Applicable > Not Applicable"; String instrument_vocabulary "GCMD Instrument Keywords"; String ISO_Topic_Categories "oceans"; String keywords "Earth Science > Human Dimensions > Natural Hazards > Tsunamis, Earth Science > Oceans > Coastal Processes > Sea Surface Height, Earth Science > Oceans > Ocean Waves > Tsunamis, Earth Science > Oceans > Sea Surface Topography > Sea Surface Height, Earth Science > Terrestrial Hydrosphere > Surface Water > Surface Water Processes/Measurements > Inundation, Earth Science Services > Models > Ocean General Circulation Models (OGCM)/Regional Ocean Models, Earth Science Services > Models > Weather Research/Forecast Models"; String keywords_vocabulary "GCMD Science Keywords"; String license "The data may be used and redistributed for free but is not intended for legal use, since it may contain inaccuracies. Neither 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 particular purpose, or assumes any legal liability for the accuracy, completeness, or usefulness, of this information."; String locations "Ocean > Pacific Ocean > Western Pacific Ocean > Micronesia > Guam > Merizo, Ocean > Pacific Ocean > Western Pacific Ocean > Micronesia > Guam > Cocos Island"; String locations_vocabulary "GCMD Location Keywords"; String metadata_link "https://www.pacioos.hawaii.edu/metadata/neowave_merizo.html"; String naming_authority "org.pacioos"; Float64 Northernmost_Northing 13.32; String platform "Models/Analyses > > Models"; String platform_vocabulary "GCMD Platform Keywords"; String program "Pacific Islands Ocean Observing System (PacIOOS)"; String project "Pacific Islands Ocean Observing System (PacIOOS)"; String publisher_email "info@pacioos.org"; String publisher_institution "Pacific Islands Ocean Observing System (PacIOOS)"; String publisher_name "Pacific Islands Ocean Observing System (PacIOOS)"; String publisher_type "institution"; String publisher_url "http://www.pacioos.hawaii.edu"; String references "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."; String source "Non-hydrostatic Evolution of Ocean WAVEs (NEOWAVE) tsunami model"; String sourceUrl "https://pae-paha.pacioos.hawaii.edu/thredds/dodsC/neowave_merizo"; Float64 Southernmost_Northing 13.22; String standard_name_vocabulary "CF Standard Name Table v39"; String summary "Non-hydrostatic Evolution of Ocean WAVEs (NEOWAVE) regional tsunami model for Merizo village and Cocos Island along the south shore of the island of Guam. Provides nearshore hazard maps of inundation depth based on preferred maximum and maximum considered earthquakes at both local and distant sources. Because tsunami waves from a local Mariana earthquake can reach Guam's shores in less than 10 minutes, the resulting inundation is considered separately from distant tsunamis, which can take at least 2 hours to reach Guam. Data are gridded at approximately 9-m (30-ft) 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."; String time_coverage_duration "P0D"; String time_coverage_resolution "P0D"; String title "NEOWAVE Regional Tsunami Model: Guam: Merizo"; Float64 Westernmost_Easting 144.63; } }
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