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Dataset Title:  Crescent City, California Tsunami Forecast Grids for MOST
Model (CrescentCityCA B), 0.0033333334°
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Institution:  NOAA OAR PMEL Center for Tsunami Research   (Dataset ID: noaa_ngdc_3b59_698d_8aa3)
Information:  Summary ? | License ? | FGDC | ISO 19115 | Metadata | Background (external link) | Make a graph
 
Dimensions ? Start ? Stride ? Stop ?  Size ?    Spacing ?
 latitude (degrees_north) ?      150    0.003333333 (even)
  < slider >
 longitude (degrees_east) ?      166    0.003333333 (even)
  < slider >
 
Grid Variables (which always also download all of the dimension variables) 
 bathy (Grid Bathymetry, meters) ?

File type: (more information)

(Documentation / Bypass this form) ?
 
(Please be patient. It may take a while to get the data.)


 

The Dataset Attribute Structure (.das) for this Dataset

Attributes {
  latitude {
    String _CoordinateAxisType "Lat";
    Float64 actual_range 41.501666666667, 41.998333333433;
    String axis "Y";
    String ioos_category "Location";
    String long_name "Latitude";
    String point_spacing "even";
    String standard_name "latitude";
    String units "degrees_north";
  }
  longitude {
    String _CoordinateAxisType "Lon";
    Float64 actual_range 235.40000000008, 235.95000000019;
    String axis "X";
    String ioos_category "Location";
    String long_name "Longitude";
    String point_spacing "even";
    String standard_name "longitude";
    String units "degrees_east";
  }
  bathy {
    Float32 _FillValue -1.0e+34;
    Float64 colorBarMaximum 8000.0;
    Float64 colorBarMinimum -8000.0;
    String colorBarPalette "TopographyDepth";
    String ioos_category "Bathymetry";
    String long_name "Grid Bathymetry";
    Float32 missing_value -1.0e+34;
    String positive "down";
    String standard_name "sea_floor_depth_below_geoid";
    String units "meters";
    String VerticalDatum "urn:x-noaa:def:datum:noaa::MHW";
  }
  NC_GLOBAL {
    String cdm_data_type "Grid";
    String Conventions "CF-1.6,ACDD-1.3, COARDS";
    String creator_email "pmel.info@noaa.gov";
    String creator_name "NOAA OAR PMEL Center for Tsunami Research";
    String creator_type "group";
    String creator_url "https://www.pmel.noaa.gov/";
    String date_created "2005-09-30";
    Float64 Easternmost_Easting 235.95000000019;
    String geospatial_bounds_vertical_crs "EPSG:5868";
    Float64 geospatial_lat_max 41.998333333433;
    Float64 geospatial_lat_min 41.501666666667;
    Float64 geospatial_lat_resolution 0.0033333333340000238;
    String geospatial_lat_units "degrees_north";
    Float64 geospatial_lon_max 235.95000000019;
    Float64 geospatial_lon_min 235.40000000008;
    Float64 geospatial_lon_resolution 0.003333333333999848;
    String geospatial_lon_units "degrees_east";
    String grid_mapping_crs_wkt "GEOGCS[\"WGS 84\",DATUM[\"WGS_1984\",SPHEROID[\"WGS 84\",6378137,298.257223563,AUTHORITY[\"EPSG\",\"7030\"]],AUTHORITY[\"EPSG\",\"6326\"]],PRIMEM[\"Greenwich\",0,AUTHORITY[\"EPSG\",\"8901\"]],UNIT[\"degree\",0.0174532925199433,AUTHORITY[\"EPSG\",\"9122\"]],AUTHORITY[\"EPSG\",\"4326\"]]";
    Float64 grid_mapping_inverse_flattening 298.257223563;
    Float64 grid_mapping_longitude_of_prime_meridian 0.0;
    String grid_mapping_name "latitude_longitude";
    Float64 grid_mapping_semi_major_axis 6378137.0;
    String grid_mapping_spatial_ref "GEOGCS[\"WGS 84\",DATUM[\"WGS_1984\",SPHEROID[\"WGS 84\",6378137,298.257223563,AUTHORITY[\"EPSG\",\"7030\"]],AUTHORITY[\"EPSG\",\"6326\"]],PRIMEM[\"Greenwich\",0,AUTHORITY[\"EPSG\",\"8901\"]],UNIT[\"degree\",0.0174532925199433,AUTHORITY[\"EPSG\",\"9122\"]],AUTHORITY[\"EPSG\",\"4326\"]]";
    String history 
"ncaedit.scm CrescentCityCA_B.nc -e nc-global:id:doi 10.7289/V50K26KT:text
2016-04-25 11:00:01 PDT: most2netcdf -x crescentcity_forecastgridsLW.xml crescent_run2d/cresc_b.txt
2024-04-18T01:02:57Z https://www.ngdc.noaa.gov/thredds/dodsC/pmel/CrescentCityCA_B.nc
2024-04-18T01:02:57Z http://upwell.pfeg.noaa.gov/erddap/griddap/noaa_ngdc_3b59_698d_8aa3.das";
    String id "pmelDatasetScan/CrescentCityCA_B.nc";
    String infoUrl "https://nctr.pmel.noaa.gov/";
    String institution "NOAA OAR PMEL Center for Tsunami Research";
    String keywords "atmospheric, bathy, bathymetry, below, california, center, city, crescent, crescentcityca, data, depth, earth, Earth Science > Oceans > Bathymetry/Seafloor Topography > Bathymetry, Earth Science > Solid Earth > Geodetics/Gravity > Geoid Properties, environmental, floor, forecast, geodetics, geoid, gravity, grid, grids, inundation model, laboratory, latitude, longitude, marine, model, most, nested grid, noaa, oar, ocean, oceanic, oceans, office, pacific, pmel, properties, research, science, sea, sea_floor_depth_below_geoid, seafloor, solid, topography, tsunami";
    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, ERD, NOAA, 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.";
    Float64 Northernmost_Northing 41.998333333433;
    String references "https://nctr.pmel.noaa.gov/sim.html";
    String source "Crescent City 1 arc-sec Digital Elevation Model, Northern California 6 arc-sec Digital Elevation Model, Northern California 36 arc-sec Digital Elevation Model";
    String sourceUrl "https://www.ngdc.noaa.gov/thredds/dodsC/pmel/CrescentCityCA_B.nc";
    Float64 Southernmost_Northing 41.501666666667;
    String standard_name_vocabulary "CF Standard Name Table v70";
    String summary "Crescent City, California Tsunami Forecast Grids for MOST Model. Pacific Marine Environmental Laboratory (PMEL) Forecast Model Grids provide bathymetric data strictly for tsunami inundation modeling with the Method of Splitting Tsunami (MOST) model. MOST is a suite of numerical simulation codes capable of simulating three processes of tsunami evolution: generation, transoceanic propagation, and inundation of dry land. Tsunami waves are computationally propagated across a set of three nested grids (A, B, and C), each of which is successively finer in resolution, moving from offshore to onshore. Nearshore details are resolved to the point that model output can be directly compared with tide gauge observations and can provide estimates of wave arrival time, wave amplitude and simulation of wave inundation onto dry land.";
    String title "Crescent City, California Tsunami Forecast Grids for MOST Model (CrescentCityCA B), 0.0033333334°";
    String version "1.0";
    Float64 Westernmost_Easting 235.40000000008;
  }
}

 

Using griddap to Request Data and Graphs from Gridded Datasets

griddap lets you request a data subset, graph, or map from a gridded dataset (for example, sea surface temperature data from a satellite), via a specially formed URL. griddap uses the OPeNDAP (external link) Data Access Protocol (DAP) (external link) and its projection constraints (external link).

The URL specifies what you want: the dataset, a description of the graph or the subset of the data, and the file type for the response.

griddap request URLs must be in the form
https://upwell.pfeg.noaa.gov/erddap/griddap/datasetID.fileType{?query}
For example,
https://upwell.pfeg.noaa.gov/erddap/griddap/jplMURSST41.htmlTable?analysed_sst[(2002-06-01T09:00:00Z)][(-89.99):1000:(89.99)][(-179.99):1000:(180.0)]
Thus, the query is often a data variable name (e.g., analysed_sst), followed by [(start):stride:(stop)] (or a shorter variation of that) for each of the variable's dimensions (for example, [time][latitude][longitude]).

For details, see the griddap Documentation.


 
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