About WSI

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  • May 15, 2013

    Introduction

    The need to acquire high density LiDAR data sets is on the rise throughout many industries. This 3D technology provides an invaluable tool for measurement, planning and assessment for projects such as the identification of geographic features, urban infrastructure mapping, and energy and safety assessments. When problem-solving with LiDAR data, it is preferable to use a data set with many survey points because a denser point cloud yields more accurate feature extraction. The native pulse density of a LiDAR data set is the number of pulses emitted by the LiDAR system, and is commonly expressed as Pulses per Square Meter (ppsm). When determining the specifications for any given LiDAR project, the questions often asked include: “What density is applicable to my study area?” In January, 2010, WSI published a white paper that described the need for a minimum of 8 ppsm data for LiDAR-based analysis in general and in the Pacific Northwest, focusing in on applications in geology, urban planning, fire modeling, and forestry. This document set a new industry standard for the quality of LiDAR data. In the time that has passed, the possibilities and applications of LiDAR data have expanded even further, as has the potential for higher quality data at more attainable costs. For modern standards in data usability, WSI recommends a minimum LiDAR density of 15 pulses per square meter (ppsm).

    Vegetation Penetration

    In regions of very thick vegetation, LiDAR sensors produce fewer ground returns because the ability of the laser to penetrate the thick canopies and branches is diminished. Acquisition with a higher pulse density increases potential ground returns, resulting in a more useful and valuable data set for any kind of analysis. In addition, when deriving tree crown polygons, performing vegetation segmentation or extracting canopy heights, there is a direct correlation between the pulse density and the quality and precision of the resulting products.

    Terrain Models

    Areas having steep terrain often require higher density LiDAR data, as deep gullies and abrupt topographic features are not often clearly represented by lower density data. Fewer pulses hitting the ground surface equates to greater interpolation between returns, and steep features may not be clearly defined within the LiDAR at 8 ppsm.

    Raster Size

    Higher resolution LiDAR data allows for a smaller raster pixel size, and therefore a sharper ground model at large scale. A sharp Digital Elevation Model (DEM) is crucial for observing and measuring small changes in ground features. When demonstrating findings of geological studies using LiDAR, a high resolution raster increases confidence in the results.

    Feature Extraction

    Above-ground features, such as human-made structures, are best represented with higher density LiDAR data because edges and angles are better defined. Creating building footprints and 3D models is most efficient and precise when derived from a point cloud with at least 15 ppsm. At this resolution, features are illuminated from more angles, creating sharper edges. For the same reason, LiDAR projects involving public utilities are also superior at higher densities. Power line infrastructure modeled for engineering applications depends on a full-bodied data set of laser returns for each transmission tower and conductor.

    Percent Illumination

    Higher density directly correlates to the percent illumination of features on and above ground level. The table below indicates percent illumination of an object’s surface compared to LiDAR pulse density. At 8 ppsm, only 56% of an object’s surface is illuminated, but at 15 ppsm the percentage doubles. At 30 ppsm, over 200% illumination is achieved.

    What Density is Appropriate?

      8 ppsm or less
    • When the terrain is flat, with little topographic relief
    • When there is a separate primary source of information
      15 ppsm or greater
    • When there is thick vegetation
    • When modeling data
    • When performing feature extraction
    • When deriving planimetric vectors

  • May 08, 2013
    On May 21st, WSI will be speaking about automated feature extraction and environmental mapping at the LiDAR & Environmental Data Forum hosted by the Sonoma County Water Agency and the Sonoma County Agricultural Preservation and Open Space District. Click Here for Registration Information .
  • April 19, 2013
    Daniel E. Coe, of Oregon's Department of Geology and Mineral Industries (DOGAMI), created a spectacular image of stream channels of the Willamette River, Oregon using a digital elevation model generated from WSI LiDAR data. To learn more, or to order a print, visit the DOGAMI website.
  • April 18, 2013
    WSI will be sharing its recent work on landslide detection, seismic hazards, hydrology/inundation modeling, and forestry biometrics at the 4th annual Bretz Club Conference on April 25th-26th in Charleston, Oregon. If you are attending, look for WSI at the poster presentation.
  • March 25, 2013

    Excerpt from Ensuring Data Quality for Alaska's North Slope. Written by James Weakland, for LiDAR Magazine.

    "The data--covering approximately 3,000 square miles along the proposed pipeline routes--were acquired to facilitate analysis during the design, permitting, and construction of the pipelines, including evaluation of active faulting, slope instability, thaw settlement, erosion, and other engineering constraints along the proposed pipeline routes. LiDAR was chosen as the preferred data format because it has proven to be one of the most useful forms of remotely sensed data for identification and characterization of potentially active faults and many other surficial-geologic landforms and hazards, especially in areas of heavy vegetation where access may be difficult and other forms of remotely sensed data are ineffective."

    Read the entire article on the LiDAR News Website, or in PDF format.

Contact Us

New Customer? Call Susan Jackson,
Chief Marketing Officer: (510) 910-8669

Portland Office: (503) 505-5100
Corvallis Office: (541) 752-1204

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