This metadata record describes the Tomales Bay grid exported as
1. ESRI ASCII grid format (includes nodata -9999 values)
ncols 3172 nrows 3959 xllcorner 501413.013329 yllcorner 4216501.279255 cellsize 4 NODATA_value -9999 -9999 -9999 -9999 -9999 -9999 -9999 -9999 -9999 -9999 -9999 -9999 -9999 -9999 -9999 -9999 -9999 -9999 -9999 -9999 -9999 -9999 -9999 -9999 -9999 -9999 -9999 -9999 -9999 -9999 -9999 -9999 -9999 -9999 -9999 -9999 -9999 -9999 -9999 -9999 -9999 -9999 -9999 -9999 -9999 -9999 -9999 -9999 -9999 -9999 -9999 -9999 -9999 -9999 -9999 -9999 -9999 -9999 -9999 -9999 -9999 -9999 -9999 -9999 -9999 -9999 -5.298165 -4.233628 -9999 -9999 -9999 -9999 -9999 -9999 -9999 -9999 -2. x-y (decimal degrees) and z (elevations in meters) data (nodata excluded).
-122.98086,38.23902,-5.298 -122.98082,38.23902,-4.234 -122.98090,38.23898,-5.162 -122.98086,38.23898,-5.997
Additional information about the field activities from which this data set was derived are available online at
<http://walrus.wr.usgs.gov/infobank/f/f104tb/html/f-1-04-tb.meta.html> <http://walrus.wr.usgs.gov/infobank/f/f205tb/html/f-2-05-tb.meta.html> <http://walrus.wr.usgs.gov/infobank/b/b106tb/html/b-1-06-tb.meta.html>Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government.
Although this Federal Geographic Data Committee-compliant metadata file is intended to document the data set in nonproprietary form, as well as in ArcInfo format, this metadata file may include some ArcInfo-specific terminology.
Anima, Roberto J. , Chin, John L. , Finlayson, David P. , McGann, Mary L. , and Wong, Florence L. , 2007, 4-m resolution bathymetric grid of Tomales Bay, California (TOMALESG): USGS Open-File Report USGS OFR 2008-1237, U.S. Geological Survey, Menlo Park, California.Online Links:
This is a Raster data set. It contains the following raster data types:
Planar coordinates are encoded using coordinate pair
Abscissae (x-coordinates) are specified to the nearest 4.0
Ordinates (y-coordinates) are specified to the nearest 4.0
Planar coordinates are specified in Meters
The horizontal datum used is WGS84.
The ellipsoid used is WGS84.
The semi-major axis of the ellipsoid used is 6378206.4.
The flattening of the ellipsoid used is 1/294.98.
TOMALESG.STA: COLUMN ITEM NAME WIDTH OUTPUT TYPE N.DEC ALTERNATE NAME 1 MIN 8 15 F 3 9 MAX 8 15 F 3 17 MEAN 8 15 F 3 25 STDV 8 15 F 3 MIN MAX MEAN STDV -19.150 0.668 -4.379 2.452
(650) 329-5327 (voice)
(650) 329-5190 (FAX)
fwong@usgs.gov
These data are intended for science researchers, students, policy makers, and the general public. The data can be used with geographic information systems (GIS) software to display geologic and oceanographic information.
The horizontal datum of the surveys was established by differential GPS using the WGS84 ellipsoid. The vertical datum of the surveys was based on Mean Lower Low Water (MLLW) predictions for Marshall, Tomales Bay, using the software Tides and Currents by Nobeltec.
Raw bathymetry and amplitude data were collected using the Swath Processor software provided with the sonar system and gridded at 1 m resolution using the accompanying Grid Processor software package. These raster data were then exported to Fledermaus, edited and smoothed in that package and finally exported to ESRI ASCII Grid format using USGS in-house software.
The horizontal and vertical datum of the survey was established by the RTK GPS system as WGS84 and NAVD88, respectively. The error ellipse on the location of the GPS receivers is typically < 5 cm and this propagates through to the sea floor with RMS errors on sea bed elevation of < 10 cm.
The advertised accuracy of the SWATHplus system in shallow waters is better than IHO S44 Special Order, but a total propagation error model has not been developed for the USGS system used in these surveys so the true error in both position and elevation is unknown. Furthermore, no operational tide measurements were available for the survey so there is likely to be a spatially and temporally variable vertical error due to differences between the predicted tides and the water levels actually experienced during the survey. Finally, a comparison of grid elevations having overlapping coverage between the 2004 and 2005 surveys revealed a 1.44 m vertical offset (median of all overlapping cells). This error may be due to a mis-configuration of the F180 unit, but the exact cause of the error is unknown. In the final DEM, a static offset of +1.44 m was added to the 2004 data to minimize the vertical offset between the 2004 and 2005 data. No additional vertical error analysis has been performed on these data.
See Attribute_Accuracy_Report.
See Attribute_Accuracy_Report.
Not applicable for raster data.
Are there legal restrictions on access or use of the data?
- Access_Constraints: None
- Use_Constraints: These data are not to be used for navigation.
(650) 329-5327 (voice)
(650) 329-5190 (FAX)
fwong@usgs.gov
USGS OFR 2007-xxx
Please recognize the U.S. Geological Survey (USGS) as the source of this information.Although these data have been used by the U.S. Geological Survey, U.S. Department of the Interior, no warranty expressed or implied is made by the U.S. Geological Survey as to the accuracy of the data.
The act of distribution shall not constitute any such warranty, and no responsibility is assumed by the U.S. Geological Survey in the use of this data, software, or related materials.
Data format: | Compressed file including Arcinfo grid and metadata. (version 9.2) Arcinfo ASCII grid Size: 5 MB |
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Network links: |
<https://pubs.usgs.gov/of/2008/1237/> |
(650) 329-5327 (voice)
(650) 329-5190 (FAX)
fwong@usgs.gov