This product set contains high-resolution Interferometric Synthetic Aperture Radar (IFSAR) imagery and geospatial data for the Barrow Peninsula (155.39 - 157.48°W, 70.86 - 71.47°N) and Barrow Triangle (156.13 - 157.08°W, 71.14 - 71.42°N), for use in Geographic Information Systems (GIS) and remote sensing software. The primary IFSAR datasets were acquired by Intermap Technologies from 27 to 29 July 2002, and consist of Orthorectified Radar Imagery (ORRI), a Digital Surface Model (DSM), and a Digital Terrain Model (DTM).
Derived data layers include aspect, shaded relief, and slope-angle grids (floating-point binary and ArcInfo grid format), as well as a vector layer of contour lines (ESRI Shapefile format). Also available are accessory layers compiled from other sources: 1:250,000- and 1:63,360-scale USGS Digital Raster Graphic (DRG) mosaic images (GeoTIFF format); 1:250,000- and 1:63,360-scale USGS quadrangle index maps (ESRI Shapefile format); a quarter-quadrangle index map for the 26 IFSAR tiles (ESRI Shapefile format); and a simple polygon layer of the extent of the Barrow Peninsula (ESRI Shapefile format).
Unmodified IFSAR data comprise 26 data tiles across UTM zones 4 and 5. The DSM and DTM tiles (5 m resolution) are provided in floating-point binary format with header and projection files. The ORRI tiles (1.25 m resolution) are available in GeoTIFF format. FGDC-compliant metadata for all data sets are provided in text, HTML, and XML formats, along with the Intermap License Agreement and product handbook.
The baseline geospatial data support education, outreach, and multi-disciplinary research of environmental change in Barrow, which is an area of focused scientific interest. The data are provided on five DVDs, available through licensing only to National Science Foundation (NSF)-funded investigators. An NSF award number must be provided when ordering data.
Manley, W. F., L. R. Lestak, C. E. Tweedie, and J.A. Maslanik. 2005. High-Resolution Radar Imagery, Digital Elevation Models, and Related GIS Layers for Barrow, Alaska. Boulder, CO: National Snow and Ice Data Center. DVD.
Please see the File List and the FGDC metadata for details about specific layers, including data sources, processing, data format, spatial and temporal resolution, extent, projection, and datum.
| Category | Description | |||
|---|---|---|---|---|
| Data format | Primary, derived, and accessory data layers are provided in different formats, including floating-point binary, ArcInfo grid, GeoTIFF, and ESRI Shapefiles. | |||
| Spatial coverage |
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| Temporal coverage and resolution | Data extend from 27 to 29 July 2002. | |||
| Tools for accessing data | These data are easily imported into ArcGIS and image processing software (ENVI, Erdas Imagine, and others). | |||
| Grid type and size | Refer to the FGDC metadata (accessed from the File List) for details specific to each layer. | |||
| File naming convention | See File List. | |||
| File size | See File List. | |||
| Parameter(s) | Elevation, terrain, radar imagery, aspect, shaded relief, slope, contours | |||
| Procedures for obtaining data | Data are available on five DVDs and are restricted to NSF-funded investigators. To place an order, visit the NSIDC catalog description for this data set. Click "Register for Data" and read the license agreement. Scroll to the end of the agreement to accept it. You will be directed to a registration form; please complete this and provide your most recent NSF grant number. NSIDC User Services will verify the grant number and contact you soon with an order confirmation. |
1. Contacts and Acknowledgments
2. Detailed Data Description
3. Data Access and Tools
4. Data Acquisition and Processing
5. References and Related Publications
6. Document Information
William F. Manley
Institute of Arctic and Alpine Research (INSTAAR)
University of Colorado
Boulder, CO, USA
Leanne Lestak
Cooperative Institute for Research in Environmental Sciences (CIRES)
University of Colorado
Boulder, CO, USA
Craig Tweedie
Arctic Ecology Laboratory
Michigan State University
Lansing, MI, USA
James Maslanik
Cooperative Institute for Research in Environmental Sciences (CIRES)
University of Colorado
Boulder, CO, USA
NSIDC User Services
National Snow and Ice Data Center
CIRES, 449 UCB
University of Colorado
Boulder, CO 80309-0449 USA
phone: +1 303.492.6199
fax: +1 303.492.2468
form: Contact NSIDC User Services
e-mail: nsidc@nsidc.org
This research was funded by the National Science Foundation Award OPP-0224071, "High-Resolution Imagery and Terrain Model for Collaborative Research of Environmental Change at Barrow, Alaska."
The National Snow and Ice Data Center (NSIDC) shall not be held liable for improper or incorrect use of the data described and/or contained herein. The information contained in these data is dynamic and may change over time. The data are not better than the original sources from which they were derived. It is the responsibility of the data user to use the data appropriately and consistently within the limitations of geospatial data in general and these data in particular. Any related graphics are intended to aid the data user in acquiring relevant data; it is not appropriate to use the related graphics as data. NSIDC gives no warranty, expressed or implied, as to the accuracy, reliability, or completeness of these data. These data and related graphics are not legal documents and are not intended to be used as such. This disclaimer applies both to individual use of the data and aggregate use with other data.
Read the Intermap license agreement.
This product set contains high-resolution Interferometric Synthetic Aperture Radar (IFSAR) imagery and geospatial data for the Barrow, Alaska, USA region for use in Geographic Information Systems (GIS) and remote sensing software packages. The baseline geospatial data support education, outreach, and multi-disciplinary research of environmental change in Barrow, an area of focused scientific interest. The data are provided on five DVDs, available through licensing only to National Science Foundation (NSF)-funded investigators. An NSF award number must be provided. Reduced-resolution versions of the data sets are available to the general public.
The primary IFSAR datasets were acquired by Intermap Technologies from 27 to 29 July 2002, and consist of Orthorectified Radar Imagery (ORRI), a Digital Surface Model (DSM), and a Digital Terrain Model (DTM). The ORRI depicts the ground surface as illuminated by airborne radar, and is useful for visualization, mapping, georectification, and a variety of analyses. The DSM is a "first-surface" reflectance model of elevation, including vegetation, buildings, and other structures. The DTM is a filtered model to better represent ground elevation, and is useful for visualization, orthorectification, and environmental analyses. Value-added products include data mosaics, derived layers, and accessory layers.
The unmodified IFSAR data comprise 26 data tiles across two UTM zones. The DSM and DTM tiles (5 m resolution) are provided in floating-point binary format with header and projection files. The ORRI tiles (1.25 m resolution) are available in GeoTIFF format. FGDC-compliant metadata created by Intermap Technologies are provided in text, HTML, and XML formats, along with the Intermap License Agreement and product handbook. The DSM, DTM, and ORRI went through rigorous quality reviews before final acceptance of the data from Intermap Technologies.
Value-added processing helped avoid redundant effort or confusion, and produced a suite of complete and consistent data. To make the primary data sets more usable, the 26 data tiles were converted to data mosaics at original 5 m resolution with a common projection (UTM Zone 4) for the spatial extent of the "Barrow Peninsula" (155.39 - 157.48°W, 70.86 - 71.47°N). The DSM and DTM mosaics are available as floating-point binary files and in ArcInfo grid format. An ORRI mosaic, at reduced resolution (5 m), is provided as a contrast-enhanced GeoTIFF file.
Processing included the creation of derived GIS layers: aspect, shaded relief, and slope-angle grids (floating-point binary and ArcInfo grid format), as well as a vector layer of contour lines (ESRI Shapefile format). Also available are accessory layers compiled from other sources: 1:250,000- and 1:63,360-scale USGS Digital Raster Graphic (DRG) mosaic images (GeoTIFF format); 1:250,000- and 1:63,360-scale USGS quadrangle index maps (ESRI Shapefile format); a quarter-quadrangle index map for the 26 IFSAR tiles (ESRI Shapefile format); and a simple polygon layer of the extent of the Barrow Peninsula (ESRI Shapefile format). To facilitate processing for a smaller area of particular interest near Barrow, each of the primary, derived, and accessory layers was clipped to a subsetted extent of the "Barrow Triangle" (156.13 - 157.08°W, 71.14 - 71.42°N).
Finally, detailed documentation was created for all of the data layers. Federal Geographic Data Committee (FGDC)-compliant metadata are provided in text, HTML, and XML formats. Please read the FGDC metadata and view the thumbnail images (accessed from the File List) for a variety of details specific to each layer or image.
| Digital Surface Model (DSM) | |
 |
The DSM is a grid of elevation measurements derived from the return signals received by two radar antennas on the aircraft. The signals bounce off the first surface they strike, making the DSM a representation of any object large enough to be resolved, including buildings, vegetation and roads, as well as natural terrain features. |
| Digital Terrain Model (DTM) | |
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The DTM is a custom "bald-earth" model that references the elevation measurements of the bare terrain. It is better suited for derived layers such as slope angle, aspect, and contours. DTM values are a result of a custom process developed for the low coastal plain of Alaska's North Slope. A repeated median filter removed most structures, as well as high-frequency noise. The DTM is well-suited for most applications of elevation analysis. |
| Orthorectified Radar Imagery (ORRI) | |
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The ORRI is a grayscale image of the first reflective surface illuminated by the radar; it was corrected to remove geometrical distortions. This radar-derived product reveals Earth surface features that are not easily identifiable with aerial photography. Furthermore, the ORRI is well suited as a base layer for georectification of aerial photography and other imagery. |
The following value-added layers are provided with the same projection, datum, and spatial extent (both Barrow Peninsula and Barrow Triangle) as the DSM, DTM, and ORRI. Please consult the metadata (accessed from the File List) provided with each layer for further details.
 Aspect |
 Slope |
 Shaded relief |
 Contours |
 mosaicked 1:250,000 scale USGS Digital Raster Graphic (DRG) |
 mosaicked 1:63,360 scale USGS DRG |
 1:250,000 scale USGS quadrangle boundaries |
 1:63,360 scale USGS quadrangle boundaries |
 Quarter quadrangles |
 Barrow Peninsula extent boundary |
The primary, derived, and accessory data layers are provided in a variety of standardized data formats, including floating-point binary, ArcInfo grid, GeoTIFF, and ESRI Shapefiles. The layers vary in terms of grid cell resolution and dimensions. For example, the DSM mosaic for the Barrow Peninsula is available in floating-point binary and ArcInfo grid formats, has grid cell spacing of 5 m, and dimensions of 13,020 rows by 14,461 columns. Please see the FGDC metadata (accessed from the File List) for details specific to each layer. To read the floating-point versions of the DSM and DTM into an image processing program, refer to the associated header files (.hdr).
Data are available on five DVDs. Please see the File List for file names, file types, file sizes, and descriptions.
Spatial extent of the Barrow Peninsula layers:
West: 157.476330°W
East: 155.394828°W
North: 71.472777°N
South: 70.862456°N
Spatial extent of Barrow Triangle layers:
West: 157.080362°W
East: 156.133882°W
North: 71.415118°N
South: 71.139168°N
The following map displays the spatial extent of the Barrow Peninsula (red lines) and Barrow Triangle (purple lines) data sets. Click the thumbnail for a larger image.
The following map displays the names and extent boundaries of IFSAR quarter quadrangle tiles as originally provided by Intermap Technologies. Use this as a reference when working with ORRI tiles (DVD 1) and unprocessed IFSAR tiles (DVD 4). Click the thumbnail for a larger image.
The following map illustrates the method for creating the IFSAR mosaics from original tiles. Click the thumbnail for a larger image.
The map projection for the Barrow Peninsula and Barrow Triangle data sets is Universal Transverse Mercator (UTM) Zone 4. Horizontal datum is the North American Datum of 1983 (NAD83). The 26 unmodified IFSAR tiles are provided in either UTM Zone 4 or UTM Zone 5. Please see the FGDC metadata (accessed from the File List) for details specific to each layer.
Intermap Technologies' STAR-3i airborne radar system collected data from 27 to 29 July 2002.
Pixel values in the DSM and DTM represent values above mean sea level (in meters). Pixels in the ORRI mosaics are greyscale values that represent magnitude of radar signal return.
Several potential sources of error exist in the DSM and DTM, as well as other layers. For more information, refer to the FGDC metadata (accessed from the File List).
Quality checks were performed throughout all processing steps. Minimum and maximum domain values were checked for each tile, for merged and mosaicked products. Map extents of separate tiles are correct. Overlaps between tiles are seamless and contain identical values; these were also spot checked for the Barrow Triangle area. Value-added layers and their ranges were quality checked; these value-added layers were also used to quality check the values in the DSM.
The vertical accuracy of DSMs and DTMs is approximately ± 1.0 m or better root-mean-square-error (RMSE). Horizontal accuracy is ± 2.5 m or better RMSE for slopes less than 20°. Horizontal accuracy of ORRI data is ± 1.25 m or better RMSE for slopes less than 20°. These accuracy statements depend on the sensor's view of the ground, and are applicable to the height of the first surface return. These statements also assume the surface is devoid of vegetation or continuous roof coverage in urban areas (Intermap 2002).
Accuracy statements are based on areas of moderate terrain. Diminished accuracies are to be expected in areas of extreme terrain and dense vegetation. The DSM and DTM contain some small (30 to 50 cm high) ripples or "corn rows." The Intermap data collection systems are very accurately calibrated to control the constant differential phase error between the antennae. The calibration ensures that data are within specification; however, on flat terrain, very low-level artifacts are present from uncompensated differential phase errors. Very small periodic DEM ripples in the range dimension occurred at a consistent location in range and are continuous along the strip. High-frequency variation (speckle) exists in both the imagery and terrain data sets. The high-frequency variation in the DEM is a product of the signal-to-noise ratio that decreases from the near to far range across the track; therefore, the noise increases with the distance from the antenna. The difference in noise between the near and far range of the strip can sometimes be seen at the seam where DEMs from two strips are mosaicked together.
Data are available on five DVDs and are restricted to NSF-funded investigators. To place an order, visit the NSIDC catalog description for this data set. Click "Register for Data" and read the license agreement. Scroll to the end of the agreement to accept it. You will be directed to a registration form; please complete this and provide your most recent NSF grant number. NSIDC User Services will verify the grant number and contact you soon with an order confirmation.
Reduced-resolution versions of these data are available to the general public.
The entire data set is approximately 16.5 GB.
NSIDC does not provide any software to read these data, which are easily imported into ArcGIS and image processing software.
The DSM, DTM, and ORRI are derived from airborne Interferometric Synthetic Aperture Radar (IFSAR). Interferometry involves detecting the radar return signal using antennas at two different locations. With an interferometric radar, the patterns of electromagnetic radiation emanating from the same point on the ground strike each antenna independently because of their different ranges. These waves are out of phase, meaning they do not always overlap each other. This phase difference result, and the geometry formed by the separation of antennas, provide all the information required to derive the height and corresponding geographic position of targets that interact with the transmitted energy (Intermap 2002).
IFSAR data were acquired from Intermap Technologies' STAR-3i airborne radar system aboard a Learjet 36A, 31,000 ft above ground level. The system transmits a radar pulse 2,200 times per second at a peak power of 8 W. Bandwidth is 135 MHz, digitization rate of the return signal is 300 million times per second, and information is recorded at 90 MB per second. The radar is mounted on a pedestal that rotates to allow the crew to collect data from either side of the aircraft, using two parallel antennas separated by 1 m. Each terrain height calculation represents the average height within the 1.25 m resolution cell (Tennant, Coyne, DeCol 2003). Acquired data are "interfered" by a digital correlation process to extract terrain height data and geometrically correct radar images. Areas of missing data are interpolated using continuous curvature spline over non-data areas. Most of these instances are due to radar shadow and layover due to steep terrain. The system's accuracy was independently validated by the U.S. Army Topographic Engineering Center, the Institute of Navigation, Stuttgart University, and by NASA.
The STAR-3i system was developed by the Environmental Research Institute of Michigan (ERIM) under contract to the U.S. Defense Advanced Research Projects Agency (DARPA).
Raw radar and navigation information are combined to produce flight strip information referenced in a radar-specific coordinate system, which are then subject to quality control (QC). Once they pass QC, the strips are transformed to the desired map projection, merged into map sheet products for elevation, radiometrically balanced, and mosaicked into map sheets (Tennant, Coyne, DeCol 2003).
IFSAR data for the Barrow region were originally delivered by Intermap Technologies as 26 tiles of data split across UTM Zones 4 and 5. Manley et al. imported the tiles into ArcInfo, merged tiles within each zone, and projected Zone 5 to Zone 4 to produce a mosaic across both zones. Data were then clipped by a Barrow Peninsula extent and a Barrow Triangle extent.
Intermap Technologies, Inc. 2002. GLOBAL terrain product handbook and quick start guide. Englewood, CO, USA: Intermap Technologies Inc.
Tennant, J.K., T. Coyne, and E. DeCol. 2003. Star-3i interferometric synthetic aperture radar (IFSAR): more lessons learned on the road to commercialization. Calgary, Alberta: Intermap Technologies Corp.
The following acronyms are used in this document:
ARCSS: Arctic System Science
BIL: Band interleaved by line
CIRES: Cooperative Institute for Research in Environmental Sciences
DARPA: Defense Advanced Research Projects Agency
DEM: Digital Elevation Model
DRG: Digital Raster Graphic
DSM: Digital Surface Model
DTM: Digital Terrain Model
ERIM: Environmental Research Institute of Michigan
ESRI: Environmental Systems Research Institute
IFSAR: Interferometric Synthetic Aperture Radar
GIS: Geographic Information Systems
NAD: North American Datum
NSF: National Science Foundation
NSIDC: National Snow and Ice Data Center
ORRI: Orthorectified Radar Imagery
QC: Quality Control
RMSE: Root-mean-square error
USGS: United States Geological Survey
UTM: Universal Transverse Mercator
February 2005
February 2005
February 2005
http://nsidc.org/data/docs/arcss/arcss302/index.html
