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GI011
LiDAR data (October 2011) for the Upper Blue River Watershed, Willamette National Forest

AUTHOR: Theresa J. Valentine
CREATOR(S): Thomas A. Spies
PRINCIPAL INVESTIGATOR(S): Thomas A. Spies
ORIGINATOR(S): Thomas A. Spies
OTHER RESEARCHER(S): Russell N. Faux
MOST RECENT METADATA REVIEW DATE:
3 Aug 2016
KEYWORDS:
Disturbance, Spatial data, stand structure, geology, geomorphology, biomass, spatial properties, topography, geographic information systems, disturbance, trees, vegetation
PURPOSE:
Study was developed as part of the LTER 6 digital forest initiative, with the cooperation of the US Environmental Protection Agency (EPA), to provide complete coverage of the Blue River Watershed (GI010 Andrews Forest and GI011 Upper Blue River).
METHODS:
Field Methods - GI011:
Description:

The LiDAR survey utilized a Leica ALS60 Phase II sensor in a Cessna Caravan 208B. The sensors operate with Automatic Gain Control (AGC) for intensity correction. The Leica systems were set to acquire 105,000 laser pulses per second (i.e. 105 kHz pulse rate) and flown at 900 meters above ground level (AGL), capturing a scan angle of ±14o from nadir. These settings were developed to yield points with an average native pulse density of 8 pulses per square meter over terrestrial surfaces. It is not uncommon for some types of surfaces (e.g. dense vegetation or water) to return fewer pulses than the laser originally emitted. These discrepancies between ‘native’ and ‘delivered’ density will vary depending on terrain, land cover, and the prevalence of water bodies.

All areas were surveyed with an opposing flight line side-lap of =50% (=100% overlap) to reduce laser shadowing and increase surface laser painting. The Leica laser systems allow up to four range measurements (returns) per pulse, and all discernible laser returns were processed for the output dataset. To accurately solve for laser point position (geographic coordinates x, y, z), the positional coordinates of the airborne sensor and the attitude of the aircraft were recorded continuously throughout the LiDAR data collection mission. Aircraft position was measured twice per second (2 Hz) by an onboard differential GPS unit. Aircraft attitude was measured 200 times per second (200 Hz) as pitch, roll and yaw (heading) from an onboard inertial measurement unit (IMU). To allow for post-processing correction and calibration, aircraft/sensor position and attitude data are indexed by GPS time.

See the complete documentation for more detail descriptions of the methodology.

Processing Procedures - GI011:
Description:

1. Resolved kinematic corrections for aircraft position data using kinematic aircraft GPS and static ground GPS data. Software: Waypoint GPS v.8.10, Trimble Geomatics Office v.1.62

2. Developed a smoothed best estimate of trajectory (SBET) file that blends post-processed aircraft position with attitude data. Sensor head position and attitude were calculated throughout the survey. The SBET data were used extensively for laser point processing. Software: IPAS v.1.35

3. Calculated laser point position by associating SBET position to each laser point return time, scan angle, intensity, etc. Created raw laser point cloud data for the entire survey in *.las (ASPRS v. 1.2) format. Software: ALS Post Processing Software v.2.70

4. Imported raw laser points into manageable blocks (less than 500 MB) to perform manual relative accuracy calibration and filter for pits/birds. Ground points were then classified for individual flight lines (to be used for relative accuracy testing and calibration). Software: TerraScan v.11.007

5. Using ground classified points per each flight line, the relative accuracy was tested. Automated line-to-line calibrations were then performed for system attitude parameters (pitch, roll, heading), mirror flex (scale) and GPS/IMU drift. Calibrations were performed on ground classified points from paired flight lines. Every flight line was used for relative accuracy calibration. Software: TerraMatch v.11.005

6. Position and attitude data were imported. Resulting data were classified as ground and non-ground points. Statistical absolute accuracy was assessed via direct comparisons of ground classified points to ground RTK survey data. Data were then converted to orthometric elevations (NAVD83) by applying a Geoid03 correction. Software: TerraScan v.11.007, TerraModeler v.11.002

7. Bare Earth models were created as a triangulated surface and exported as ArcInfo ASCII grids at a 1 m pixel resolution. Highest Hit models were created for any class at 1 m grid spacing and exported as ArcInfo ASCII grids. Software: TerraScan v.11.007, ArcMap v. 9.3.1, TerraModeler v.11.002

Processing Procedures - GI011 (1):
Description: Raw DEM's were processed using ArcGIS 10.1 desktop software. Aspect, percent slope, flow accumulation, and hill shade grids were produced using standard methods. 10, 25, and 50 meter contours were produced using generalized 10 meter DEM's and smoothed.
TAXONOMIC SYSTEM:
None
GEOGRAPHIC EXTENT:
Oregon, Willamette Basin, Blue River Watershed, Upper Blue River Watershed
ELEVATION_MINIMUM (meters):
401
ELEVATION_MAXIMUM (meters):
1631
MEASUREMENT FREQUENCY:
as needed
PROGRESS DESCRIPTION:
Complete
UPDATE FREQUENCY DESCRIPTION:
notPlanned
CURRENTNESS REFERENCE:
Observed