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The precipitation data are quality-controlled, multi-sensor (radar and rain gauge) precipitation estimates obtained from National Weather Service (NWS) River Forecast Centers (RFCs) and mosaicked by National Centers for Environmental Prediction (NCEP). The original data from NCEP is in GRIB (GRIdded Binary or General Regularly-distributed Information in Binary form) format (files pre-March 22nd, 2017 are in XMRG format) and projected in the Hydrologic Rainfall Analysis Project (HRAP) grid coordinate system, a polar stereographic projection true at 60N / 105W.
In all three masks, a value of 0 marks a cell that does not fall within the bounds of valid input data. A three digit value will indicate which RFC is responsible for providing data for a given grid cell. In many cases, any value greater than 1 can simply be considered a cell which should contain valid data. Lastly, the CONUS mask contains cells with a value of 1. These cells indicate they contain offshore readings from coastal RFCs. A value of 1 fills the cells in the Gulf of Mexico and of the eastern coastline of the United States.
A problem was discovered on August 9, 2007. The shapefile coordinates for each HRAP grid were indicative of the lower left corner of the grid rather than the center of the grid. The entire shapefile archive has been updated to correct the lat-lon issue. The shapefile _precip_allpoint_conversion.tar.gz shows both the old and new coordinates for each point.
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The downloadable products include sufficient information to reproduce theShakeMap. In particular, stationlist.xml and the *_fault.txt file(s) provide theinput files, grid.xml provides the Vs30 grid (see above), and info.xmlprovides the important configuration and processing parameters, including thename(s) of the fault file(s).
Because the ShakeMap output grid is the fundamental derived product from the ShakeMapprocessing, it is fully described in an accompanying metadata file followingFederal Geographic Data Committee (FGDC) standardsfor geospatial information. As described below, station amplitudes are providedin separate ShakeMap station files; however, the complete metadata for the parametric data arearchived by the regional seismic networks and contributing strong-motion datasources.
Figure 7: Interactive ShakeMap for the 2014 M6.0 American Canyon, CAearthquake. On the interactive map, reported (DYFI) intensities are geocoded and represented withsquares depicting the 1km grid area they occupy. Reported Intensities are color-coded according to their intensityvalue, either as observed or as converted by Wald et al. (1999b).
As described in the Technical Guide, the fundamental output product of theShakeMap processing system is a finely-sampled grid (nominally 1kmspacing) of latitude and longitudepairs with associated amplitude values of shaking parameters at each point.These amplitude values are derived by interpolation of a combination of therecorded ground shaking observations and estimated amplitudes, with considerationof site amplification at all interpolated points. The resulting grid ofamplitude values provides the basis for generating color-coded intensity contourmaps, for further interpolation to infer shaking at selected locations, and forgenerating GIS-formatted files for further analyses.
XML Grid. The ShakeMap XML grid file is the basis for nearly all ShakeMapproducts, as well as for computerized post-processing in systems such asShakeCast and PAGER [see Related Systems]. The XML grid is availableas both plain text (grid.xml) and compressed as a zip file(grid.xml.zip). As XML, the grid is meant to be self-describing; however, we describe the formathere for the sake of completeness.
The number of grid_field tags will vary: smaller-magnitude earthquakes may nothave the pseudo-spectral acceleration values; scenarios will not have STDPGA orURAT; and maps that have not been site corrected will not have SVEL.
The fast index for the coordinates is longitude, the slow index is latitude.Dimensions are from upper left to lower right (i.e., from longitudeminimum/latitude maximum to longitude maximum/latitude minimum). The GMT programxyz2grd (coupled with gmtconvert) is particularly useful for converting thegrid.xml data into a usable grid file.
Rock Grid XML. The file rock_grid.xml.zip is a zipped XML file containingthe interpolated grid without site amplifications applied. The rock grid has thesame structure as grid.xml, but Vs30 values and PGA uncertainty values are notsupplied. Amplify Ground Motions in the Technical Guide.
Uncertainty Grid XML. The file uncertainty.xml.zip is a zipped XML filecontaining the standard errors for each of the ground-motion parameters at eachpoint in the output grid. It has the same structure as grid.xml, with theadditional grid_field names:
The standard errors are given in natural log units, except for intensity (linearunits). The PSA entries will be available only if the PSA ground motionparameters were mapped (typically only for earthquakes of M >= 5.0). Noground motion data or Vs30 values are available inuncertainty.xml.zip; for those, use grid.xml.zip.
The use of grid.xyz is deprecated. It is difficult to maintain and have it remain backward-compatible. All users are urged to use the XML grids instead, and to switch to the XML grids if they are using grid.xyz. grid.xyz will disappear in a future ShakeMap release.
ShakeMap GIS Files (zipped) are a collection of shapefiles of polygons of theShakeMap model outputs for each shaking metric: MMI, PGA, PGV, and PSA at threeperiods (0.3, 1.0, and 3.0 sec). These file should be easily importable into a GISsystem. The ESRI RasterFiles (also zipped) are a collection of ESRI-formatted binary files. It shouldbe relatively easy to convert these to (for example) ArcGIS grids using thestandard tools provided with the software. The contours are useful primarily foroverlaying with other data for visualization purposes.
ESRI raster grids of the ground-motionparameters and their uncertainties are also available. The files are found in azipped archive called raster.zip. Each archive contains four files perparameter: .flt and .hdr, which contain the ground-motiondata, and _std.flt and _std.hdr, which contain theuncertainties for the ground motions. See grid.xml for information on units.As with the other GIS files, PGA, PGV, and MMI are available for all events,while the PSA parameters are usually only included for earthquakesM4.5 and larger.
In some situations, you could be interested in exporting only the grid data, without exporting the header cells. For this scenario, we provide the skipColumnGroupHeaders=true and skipColumnHeaders=true params. 041b061a72