Lidar and the Oregon Lidar Consortium

Slides:



Advertisements
Similar presentations
Reality Check: Processing LiDAR Data A story of data, more data and some more data.
Advertisements

Mapping (Topographic) Surveys
High Accuracy Helicopter Lidar & Mapping Jeffrey B. Stroub, CP,RLS,PPS,SP Vice President Business Development September 9, 2014 Jeff Stroub CP, RLS, PPS,
Spatial Analysis with ArcView: 2-D. –Calculating viewshed –Calculating line of sight –Add x and y coordinates –Deriving slope from surface data –Deriving.
Applied Geographics, Inc./Tennessee Regional Forums/Enhanced Elevation/August 2011Slide 1 Tennessee Business Planning Technical Overview on Enhanced Elevation.
Brian S. Keiling Program Head – Forest Management Dabney S.Lancaster Community College.
Mapping.
Topographical Maps.
Topographic maps show…. - USGS: Uses for topographic maps… -
Technology Enables Us To Explore Our Earth The Land and the Oceans.
Lesson Objectives 12/2/13 TLW, with 100% participation,
FOR 474: Forest Inventory LiDAR for DEMs The Main Principal Common Methods Limitations Readings: See Website.
FOR 474: Forest Inventory Plot Level Metrics from Lidar Heights Other Plot Measures Sources of Error Readings: See Website.
From Topographic Maps to Digital Elevation Models Daniel Sheehan DUE Office of Educational Innovation & Technology Anne Graham MIT Libraries.
Modeling Digital Remote Sensing Presented by Rob Snyder.
Airborne LIDAR The Technology Slides adapted from a talk given by Mike Renslow - Spencer B. Gross, Inc. Frank L.Scarpace Professor Environmental Remote.
From Topographic Maps to Digital Elevation Models Daniel Sheehan IS&T Academic Computing Anne Graham MIT Libraries.
TRYPHINE DUDZAYI.  Surveying instrumentation has undergone a major transformation over the past years transit to the modern instruments.  The theodolite,
Comparison of LIDAR Derived Data to Traditional Photogrammetric Mapping David Veneziano Dr. Reginald Souleyrette Dr. Shauna Hallmark GIS-T 2002 August.
1. LiDAR Mapping Light Detection and Ranging (LiDAR) mapping provided for the United States International Boundary and Water Commission (USIBWC) – established.
An Introduction to Lidar Mark E. Meade, PE, PLS, CP Photo Science, Inc.
Adams County Lidar Project
Dave Tewksbury Department of Geosciences Hamilton College Clinton, NY On the Cutting Edge Albuquerque 2013.
Esri International User Conference | San Diego, CA Technical Workshops | Lidar Solutions in ArcGIS Clayton Crawford July 2011.
Lecture 17 – Forest remote sensing  Reading assignment:  Ch 4.7, 8.23,  Kane et al., Interpretation and topographic correction of conifer forest.
TOPOGRAPHIC MAP.
Accessing LIDAR GIS day 2012 Larry Theller ABE Purdue University.
UNDERSTANDING LIDAR LIGHT DETECTION AND RANGING LIDAR is a remote sensing technique that can measure the distance to objects on and above the ground surface.
APPLICATION OF LIDAR IN FLOODPLAIN MAPPING Imane MRINI GIS in Water Resources University of Texas at Austin Source. Optech,Inc.
Digital Terrain Models by M. Varshosaz
Hydro-enhancement of LiDAR Data to Support Floodplain Modeling 2011 ASFPM Annual Conference Louisville, Kentucky May 18, 2011 Mark W. Ellard, PE, CFM Associate,
Quantitative Estimates of Biomass and Forest Structure in Coastal Temperate Rainforests Derived from Multi-return Airborne Lidar Marc G. Kramer 1 and Michael.
Karst Topography – Developing a Sinkhole Inventory to Protect Groundwater Quality Presenters: Stacey Jarboe and John-Paul Brashear Stantec Consulting Services.
Chapter 3 Section 1- Finding Locations on Earth
STRATIFICATION PLOT PLACEMENT CONTROLS Strategy for Monitoring Post-fire Rehabilitation Treatments Troy Wirth and David Pyke USGS – Biological Resources.
U.S. Department of the Interior U.S. Geological Survey Elevation Data Product Needs and Requirements Larry Sugarbaker Senior Advisor - Geography.
LIDAR Technology Everett Hinkley USDA Forest Service Geospatial Management Office Prepared for Congressman Allan Mollahan's Office.
Uses of Geospatial Soils & Surface Measurement Data in DWR Delta Levee Program Joel Dudas
RASTERTIN. What is LiDAR? LiDAR = Light Detection And Ranging Active form of remote sensing measuring distance to target surfaces using narrow beams of.
Using LiDAR to map sinkholes in Jefferson County, West Virginia John Young, USGS Leetown Science Center Kearneysville, WV.
LIDAR – Light Detection And Ranging San Diego State University.
TLW, with 100% participation Identify landforms on a topographic map Use contour lines to interpret terrain features and elevation Apply knowledge of weathering.
A bestiary of lidar errors The following images illustrate some of the defects that may be found in lidar-derived bare-earth models. The images also illustrate.
Topographic Maps TOPOGRAPHIC MAPS. Topographic map is a model, which attempts to show a 3-D world in a 2-D format.
Lidar distribution system for OLC lidar Rudie Watzig, Senior GIS Analyst Oregon Dept. of Geology and Mineral Industries Framework Review Committee, April.
LiDAR Remote Sensing of Forest Vegetation Ryan Anderson, Bruce Cook, and Paul Bolstad University of Minnesota.
Mapping. What is a map? It is a representation of something (Earth, stars, solar system, a building, etc… It is a representation of something (Earth,
Remote Sensing of Forest Structure Van R. Kane College of Forest Resources.
SGM as an Affordable Alternative to LiDAR
FOR 274: From Photos to Lidar Introduction to LiDAR What is it? How does it work? LiDAR Jargon and Terms Natural Resource Applications Data Acquisition.
Topographic maps EQ: Why does the surface of the Earth change? Starter: 1/21/ Topographic maps 1/21/2016 Practice: Write observations here.
Part 2:Topographic Maps Essential Questions: How can scale, distance, slope, relief, and profiles be determined from analyzing topographic maps? Essential.
In complete sentences, describe three (3) ways you have used maps.
Field Drainage Technology LiDAR John Nowatzki Extension Ag Machine Systems Specialist.
Washtenaw County 2008 LiDAR Project Overview Nate Arnold, GIS Developer Washtenaw County Support Services
U NIVERSITY OF J OENSUU F ACULTY OF F ORESTRY Introduction to Lidar and Airborne Laser Scanning Petteri Packalén Kärkihankkeen ”Multi-scale Geospatial.
An Accuracy Assessment of a Digital Elevation Model Derived From an Airborne Profiling Laser Joseph M. Piwowar Philip J. Howarth Waterloo Laboratory for.
Cartography The study of maps and map making. Types of Map Projections.
Essential Questions - Topography
Integrated spatial data LIDAR Mapping for Coastal Monitoring Dr Alison Matthews Geomatics Manager Environment Agency Geomatics Group.
Integrating LiDAR Intensity and Elevation Data for Terrain Characterization in a Forested Area Cheng Wang and Nancy F. Glenn IEEE GEOSCIENCE AND REMOTE.
Counting the trees in the forest
Interpreting a contour map
Mapping.
How to Read Topographic Maps Natural Resources Engineering
Lidar Image Processing
Washington Geological Survey
Why might this map be useful?
Take Notes as you view the slides
Topographic Survey Introduction „ Mapping surveys are made
Presentation transcript:

Lidar and the Oregon Lidar Consortium Beaverton: photo and lidar highest hit model Portland State Office Building: photo and lidar point cloud Eagle Creek landslides, abandoned railroad: photo and bare earth model

What is lidar (light detection and ranging) What is lidar (light detection and ranging)? - Simply making lots of accurate distance measurements with a laser rangefinder. Accurate laser rangefinders are commonly used as surveying instruments, measuring tapes, rifle scopes, even golf aids! Distance is calculated by measuring the time that a laser pulse takes to travel to and from an object.

Millions of very precise laser range measurements are made from a precisely located aircraft, producing an accurate and detailed 3-D map of the earth’s surface, as a “point cloud.” On-ground RTK-GPS base stations broadcast corrections to airborne GPS unit, locating the aircraft with an accuracy of a few centimeters. Aircraft attitude is precisely measured by Inertial Motion Unit, so that the exact position and orientation of the laser rangefinder is always known. The rangefinder scans across the surface at 100,000 to 200,000 pulses per second, collecting millions or billions of precise distance measurements, which are converted to 3-D coordinates.

Point cloud data define the 3-D shape and location of the land, vegetation, and structures. The complete collection of measured points for an area is called the point cloud, which is the fundamental form of lidar data. It provides a very detailed and accurate 3-D map of ground surface, vegetation, and structures. (above) Animated point cloud image of the Portland LDS Temple; points are colored by their relative height: red highest, blue lowest. (right) Photo of the same building; note statue on left hand spire, visible in both images.

Each laser pulse can produce multiple consecutive measurements from reflections off several surfaces in its path. This provides detailed images of vegetation structure and density, and returns data from the ground under tree cover. Image on the left is a point cloud lidar view of the tree in the photo on the right. Each point is colored by which return it was from a particular pulse: red= 1st return yellow = 2nd return green = 3rd return

OLC data are collected at very high pulse density, producing very detailed images. Point cloud image on left compared to orthophoto on right shows actual point density of lidar data acquired over school bus lot. Each bus has been measured by 180-200 lidar points!

The lidar point cloud can even image livestock in the field! Red and yellow clusters of points above ground are cattle standing or lying in pasture.

For comparison, the best previously available ground model is shown on the left. The 10-m USGS Digital Elevation Model shows only a crude representation of the real surface. Even if only one point in one hundred is a ground point, the huge number of points means that a smooth seamless ground model can be made. The image on the left is a bare earth digital elevation model, with 3 ft pixels, and reveals incredible detail of the terrain beneath the trees, including a hidden landslide. The lidar vendor uses a variety of software filters to choose the points out of the point cloud that measure the ground surface. In the image on the right, vegetation points are green and ground points yellow. Even in thick forest there are numerous ground points. Very high point density means that even in heavily forested areas, it is still possible to get a large number of measurements of the ground. Left image is orthophoto of the Tualatin River, right image is lidar point cloud with red points high, blue points low.

Arrows connect matching locations. Bare earth lidar can show features that you cannot even see on the ground. Perspective view of lidar (Dec. 2007) on left matches photograph (July 2008) on right. The lidar was flown before clear cut logging of the reddish-brown slope, yet clearly shows an old logging road that is barely visible in the photograph. Arrows connect matching locations.

Additional standard lidar products include a “highest hit” or “first returns” model, which shows the tops of trees and buildings, and an intensity image, which is a form of infrared photograph. True color orthophoto with 0.5 ft pixels Lidar highest hit model with 3 ft pixels Lidar intensity image with 1 ft pixels Transmission lines Nursery stock Residence Quarry Auto

Lidar data allow a wide variety of information about forests to be measured with unprecedented accuracy and completeness. Tallest tree at 252 ft! Locate and measure individual trees in forest Estimate fuel loads, carbon content, timber volume Tell conifer from deciduous Identify damaged forest 150-250 ft forest 60-100 ft forest Image at right shows a simple analysis, subtracting the bare earth surface model from a first return (highest hit) surface model to produce a canopy height model. Low canopy is violet, high is red. The shapes of individual trees are apparent, and the tallest tree in the forest can be easily found and measured. 135-190 ft forest 100-125 ft forest Brush and grass 40-60 ft forest 50-80 ft forest

Comparing the highest hit or surface and bare earth surface provides a detailed and accurate model of building area and height Building, 9,000 sq ft, 27 ft high Building, 4,900 sq ft, 11 ft high Residence, 2,300 sq ft, 12 ft high Building, 19,850 sq ft, 89 ft high Building, 16,750 sq ft, 79 ft high Light standards, 54 ft high Building, 20,100 sq ft, 155 ft high Overpass, 23 ft high Highway sign, 27 ft high Powerline, 56 ft high Parking structure, 79,400 sq ft, 3-20 ft high, sloped for drainage

The lidar image can show where existing maps are inaccurate The highly detailed bare earth model allows for accurate location of roads and provides easy access to unprecedented levels of detail about slopes and shapes Yellow lines are best current digital road map. The lidar image can show where existing maps are inaccurate Because the bare earth model contains detailed information about the shape of the land surface, it is easy to construct a profile across a road to examine its construction and condition Drainage ditch on uphill side Roadcut not too steep Properly crowned for drainage or show where mapped roads do not exist or locate roads that are not on existing maps

Stream channels are readily apparent on lidar bare earth images Comparing the lidar-derived streams with the current digital stream map shows that the current data are often wildly inaccurate Dark blue lines are best current digital stream map, light blue are lidar-derived. GIS software can automatically find stream channels from lidar data Blue lines are streams generated by ArcGIS misses sinuous channel, climbs ridges Crosses divide, mouth wildly off cross divides

In addition to accurately locating streams, lidar easily produces accurate and detailed profiles and sections Light blue line is lidar derived stream location, dark blue are section lines. A detailed elevation profile down the stream shows areas of steep or gentle grade, waterfalls and pools. Culverts at road crossing show up as upward blips on the profile. Stream section shows distinct floodplain and channel Section shows “v” shape of rapidly downcutting stream

What can you do with lidar? You can quickly, cheaply, and accurately…. Find landslides, old cuts and grades Measure and estimate fills and cuts Find stream channels, measure gradients Measure the size and height of buildings, bridges Locate and measure every tree in the forest Characterize land cover Model floods, fire behavior Locate power lines and powerpoles Find archeological sites Map wetlands and impervious surfaces Define watersheds and viewsheds Model insolation and shading Map road center and sidelines Find law enforcement targets Map landforms and soils Assess property remotely Inventory carbon Monitor quarries, find abandoned mines Enhance any research that requires a detailed and accurate 2D or 3-D map

The Portland Lidar Consortium was the first large scale effort to collect lidar in Oregon. “Hood to Coast” survey In 2003, the USGS funded DOGAMI for a pilot lidar survey to look for earthquake faults. With the USGS funds to anchor the survey and ensure a large enough area for the lowest possible rate, Federal, State and local government agencies added on their areas of interest until the entire project had grown to over 2300 square miles and $1.1 M, with over 20 funding partners. In 2006, the USGS provided DOGAMI with $100k to complete the City of Portland. DOGAMI formed the Portland Lidar Consortium to develop funding partnerships to increase the area. This was followed in 2005 by another USGS-DOGAMI flight in the Portland Hills, a USGS survey of the Columbia River Floodplain, and a survey by Oregon City of its urban growth boundary.

The Oregon Lidar Consortium (OLC) originated in 2007 with a request by DOGAMI to the 2007 legislature for funds to acquire lidar over the inhabited parts of Western Oregon. The legislature provided $1.5 M of the 4.5 M request and encouraged DOGAMI to seek funding partners to increase coverage The relatively small amount of funding requires prioritization to areas with significant local contributions Blue hatch at left shows the original $4.5 M target based on the inhabited area of Western Oregon. Red hatch shows the area that could be covered by $1.5 M, magenta shows existing data.

DOGAMI Business Plan for the OLC Collection areas should be large and contiguous Collection areas initially anchored by significant contribution from local funding partner OLC builds on anchor funding by finding additional partners State funds used to knit together partner areas State funds are spent on the inhabited areas of the state Collection areas completely outside the inhabited areas are fine if fully partner funded Data in public domain Where possible, collection areas should include entire 6th field watersheds

DOGAMI selected a vendor to provide lidar to the consortium. A nationwide RFP led to the selection for Watershed Sciences Inc. of Corvallis, Oregon, as the lidar vendor for the consortium under Oregon Price Agreement 8865. Watershed Sciences

OLC lidar prices are a function of area OLC lidar prices are a function of area. DOGAMI adds 10% to the vendor price for quality control and management.

Data Specifications Laser spot size on ground 15-40 cm 1m Aggregate pulse density > 8/m2 Absolute accuracy of each point 20 cm horizontal and vertical 50% sidelap for complete double coverage 1m Swath to swath consistency 15 cm (same point measured by adjacent swaths must have similar value) Point cloud image of field and building: red points are from one swath, blue from another.

DOGAMI provides three-way independent quality control for OLC data. OLC lidar image showing DOGAMI quality control points (red triangles) collected by RTK-GPS survey. Compare accurately surveyed control points to the final lidar product to test absolute accuracy (+/- 20 cm). Colors indicate data from different swaths “Bird” anomalies produce spikes in bare earth model Compare adjacent points from overlapping swaths to test consistency (+/- 15 cm) GPS elevation = 50.40 m Lidar elevation = 50.38 m Error = 2 cm Inspect bare earth models for artifacts, processing errors Lidar production software is used to automatically compare locations for huge numbers of points from overlapping swaths. Swath to swath differences, measured on hundreds of thousands of points per swath, average about 3 cm in this example

OLC Data Products 3 ft pixel first return DEM ESRI format (quad tiles) 3 ft pixel bare earth DEM ESRI format (quad tiles) Point cloud, LAS format 1/100 quad tiles 1 ft pixel intensity images (1/4 quad tiles) Ground points in LAS format (1/100 quad tiles) Aircraft trajectories Report and metadata !!

Data Distribution Options Funding partners: Copies are provided on external hard drives as soon as DOGAMI completes QC. Public: NOAA LDART website (point cloud) USGS CLICK website (point cloud) USGS NED website (DEM) GEO spatial data library website (DEM) METRO (Portland area only) PSLC (“Hood to Coast” area only) DOGAMI website (planned) DOGAMI publications on disk or drive (planned)

As of September 2008, 25 partners have added $2 As of September 2008, 25 partners have added $2.7 million to the Oregon Legislature’s $1.5 million. The City of Philomath The City of Turner http://www.lincolncity.org/Portals/29/logo2.gif

As of September 2008, the OLC has been successful in building partnerships for several lidar collections around the state. Current status at http://www.oregongeology.com/sub/projects/olc/default.htm

Future Plans DOGAMI is seeking funds in future biennia to extend coverage to other parts of the state, as illustrated in the conceptual draft below.