Finlayson, David, 20040131, Sources for the Combine Bathymetry and Topography of the Puget Lowlands, Washington (January 2005) digital elevation model.Online Links:
This is a Raster data set. It contains the following raster data types:
The map projection used is Lambert Conformal Conic.
Planar coordinates are encoded using row and column
Abscissae (x-coordinates) are specified to the nearest 30.000000
Ordinates (y-coordinates) are specified to the nearest 30.000000
Planar coordinates are specified in survey feet
The horizontal datum used is North American Datum of 1983.
The ellipsoid used is Geodetic Reference System 80.
The semi-major axis of the ellipsoid used is 6378137.000000.
The flattening of the ellipsoid used is 1/298.257222.
| Value | Definition |
|---|---|
| 1 | No source for this elevation value. The value was interpolated during the construction of the DEM |
| 2 | Terrapoint, Inc. (2000-2004) LIDAR topography of the Puget Lowlands. Under contract with the Puget Sound Lidar Consortium (LIDAR) |
| 3 | Troost, Kathy (unpublished) Digital contours of Lake Washington. The Pacific Northwest Center for Geologic Mapping. Unviersity of Washington, Seattle, WA (Digitized Contours?) |
| 4 | Haugerud, Ralph (2003) Composite grids of SHOALS bathymetric LIDAR data. US Geological Survey (LIDAR Bathymetry) |
| 5 | Greenberg, Harvey (2001) 10-meter DEM composite of the USGS 10-meter DEM series for Washington State. Earth and Space Sciences, University of Washington, Seattle WA (Digitized Contours?) |
| 6 | Gregg, Mike (2002) R/V Thompson Cruise TN146 and TN147. Applied Physics Laboratory, University of Washington, Seattle WA (Swath Bathymetry) |
| 7 | Gardner, J. (2001) Multibeam mapping the major deltas of southern Puget Sound, WA from Field Activity: R-1-01-WA. US Geological Survey, Coast and Marine Geology (CMG) (Swatch Bathymetry) |
| 8 | David Evans and Associates, Inc. (2004) Lower Duwamish waterway bathymetric survey (swath bathymetry). under contract to the US Environmental Protection Agency and WA ST. Dept. of Ecology. (Swath Bathymetry) |
| 10 | Tenix LADS Corp. Near-shore bathymetry for the Puget Sound Lidar Consortium. Under contract to the Puget Sound Lidar Consortium. (LIDAR bathymetry) |
| 11 | Gelfenbaum, Guy (2001) Nearshore LIDAR bathymetry of Camano Island, Puget Sound, WA. US Geological Survey (LIDAR bathymetry) |
| 12 | Office of the Coast Survey (1931-2000) National Ocean Service Office of the Coast Survey Hydrographic Survey Data. NOAA National Ocean Service (digitized soundings) |
Funding for this project was provided by Washington SeaGrant and the U.S. Army Corps of Engineers. A Special thank you to Ralph Haugerud, Harvey Greenberg and Elizabeth Cassel without whose assistance this DEM could not have been completed. Most importantly, this project relies on Public Domain elevation data provided by the Puget Sound Lidar Consortium (PSLC), the U.S. Geological Survey (USGS), the National Ocean Service (NOS), the University of Washington (UW), and the Lower Duwamish Working Group (LDWG). Please support public access to publicly funded data so that projects like this can be made possible.
(206) 616-9407 (voice)
dfinlays@u.washington.edu
The purpose of this raster is two fold: (1) to identify the source of each elevation value in the PSDEM, (2) to make it easy to update the DEM for future maintainers.
David Finlayson, School of Oceanography, University of , 20050127, Combined bathymetry and topography of the Puget Lowlands (January 2005).Online Links:
The reported source ID was assigned by differencing the PSDEM after each processing step. This should result in perfect correlation between the source raster and the original DEM. This has not been checked.
The horizontal accuracy of this DEM has not been tested.
The horizontal accuracy is a function of the accuracy of the various underlying data sets plus the errors introduced during the production of this DEM (including reprojecting, resampling and adjusting the horizontal datum). With the exception of the NOS conventional soundings, all data sources had a higher horizontal resolution than the 30-foot resolution for this DEM. A best-guess would be that cell values are accurate to within 1-cell spacing (30-feet)
There are no intentional data gaps in this converage. Every cell in the PSDEM 2005 should have a source value in this map.
Because this raster can only hold one data value per cell, it follows that only one data source can be associated with each cell. In many places in the DEM two data sources were blended together to smooth the margins between data, especially if the transition was from a high resolution source to a low resolution source. The policy followed on land (NAVD88 > 0), was to record only the lowest resolution source. The policy on the water (NAVD88 <= 0) was to record the highest resolution source. This later situation is regrettable, but irreversible without rebuilding the DEM. To make matters somewhat better, the overlap between the NOS bathymetry and the swath bathymetry was always 300 feet from the edge. This region should be flagged as having a hybrid source.
For all data sources except the NOS bathymetry, the source data was of equal or higher spatial resolution than the DEM (30-foot). So, for these datasets I assigned every cell within the data hull to the source. The NOAA bathymetry however was of much lower resolution. In the deeper parts of the Sound the spacing between soundings can be on the order of 2000 ft or more. I chose to identify only those cells within a 200 foot range of a sounding as belonging to NOAA, the remaining values were assigned to my interpolation class.
Are there legal restrictions on access or use of the data?
- Access_Constraints:
- This work is licensed under the Creative Commons Attribution License. To view a copy of this license, visit <http://creativecommons.org/licenses/by/2.0/> or send a letter to Creative Commons, 559 Nathan Abbott Way, Stanford, California 94305, USA.
- Use_Constraints: None
(206) 616-9407 (voice)
dfinlays@u.washington.edu
Downloadable Data
Although these data have been processed successfully on a computer system at the University of Washington, no warrenty expressed or implied is made by the University of Washington regarding the utility of the data on any other system, nor shall the act of distribution constitude any such warranty.
| Data format: | Size: 10.109 |
|---|
These data are available for download at <http://www.ocean.washington.edu/data/pugetsound/>
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(206) 616-9407 (voice)
dfinlays@u.washington.edu