Pilot project to calibrate ICESat satellite laser data with airborne LiDAR. Developing a new dataset for forest height and cover across Australia Alex Lee1, Peter Scarth2, Adam Gerrand3. 1. The Fenner School, Australian National University and DIGO 2. Queensland government SLATS team, QDNRW. 3. Bureau of Rural Sciences
Pilot Project Aims To investigate the Australian use of ICESat satellite laser data for the National Forest Inventory, to improve forest sampling of height and cover, national reporting and monitoring.
Collaboration between the Queensland government Statewide Land and Tree Survey (SLATS) team, ANU, BRS, and CSIRO.
SLATS investigating ICESat data to help improve their Foliage Projective Cover (FPC) and vegetation change detection processes CSIRO looking at ICESat data to improve continental DEM derived from satellite radar, with potential for vegetation height layer.
What is ICESat?
ICESat (Ice, Cloud, and land Elevation Satellite) is a spaceborne LIDAR platform, primarily used to measure ice change at the poles, using the Geoscience Laser Altimeter System (GLAS) The laser transmits very short pulses of infrared light and visible green light Photons reflected back to spacecraft from Earth and from the atmosphere, including the inside of clouds, collected in a 1 metre diameter telescope. Laser pulses at 40 times per second will illuminate spots (footprints) approximately 70 meters in diameter, spaced at 170-meter intervals Data is free to download from NASA ~ ICESat website: http://ICESat.gsfc.nasa.gov/)
What does the data look like? GLAS received waveform (below, red) typical of returns from tree cover on flat ground transmit pulse waveform is 7 ns (1 m) wide at half the maximum amplitude (black), and alternate threshold (dotted line), alternate signal start & end (horizontal blue lines) and centroid (horizontal dashed blue line), ‘‘standard’’ Gaussian fit and centroid (black dashed line), ‘‘alternate’’ fits (cyan), & alternate model fit from sum of alternate Gaussians (thick blue line) Received waveform & transmit pulse amplitudes are scaled separately Tree cover shown is illustrative; it does not correspond to the location of the waveform.
Where is the data collected?
Transects approx 25km apart (vary 500m - 75km)
Data collected approx every 6 months since Jan 2003
Variation in lasers mean that shift in data collection (appears transects are “moving” west to east) -> 50-500m offset for subsequent collection periods
ICESat Calibration – NE Victoria
27 overlap locations
94 footprints within airborne LiDAR
Range of environments: • Floodplain forests • Foothills grazed woodlands • Montane tall forests
Project primary calibration site
ICESat Calibration – Injune, central Qld • 18 footprints within airborne LiDAR • Airborne LiDAR located within 150 500 x 150m sampling units. Study area is 220,000ha in total • Foothills grazed woodlands and open forests • dominated by Eucalypt (poplar box, ironbarks) and • Callitris species, with • Angophora, & Acacia also present (mainly brigalow). • Secondary calibration site.
ICESat Calibration – SE Queensland Brisbane River Lidar – 20 footprints overlap airborne LiDAR at 5 locations
SEQ Private Native Forest project lidar – approx 11 overlap locations. Airborne LiDAR not yet checked for number of footprints
ICESat Calibration – Other potential locations Near Mt Isa
AAMHatch intersected ICESat footprints with their existing LiDAR holdings (for 2006)
Near Townsville
Near Rockhampton
Bundaberg Near Toowoomba
Additionally, SLATS team have ongoing LiDAR calibration sites throughout Queensland
Near Coober Pedy Near Grafton
Near Walgett
Near Taree Near Dubbo Near Mildura Near Hay
Wimmera Mallee Pipeline project
Near Kingston SE Near Lismore
Near Bunyip
ICESat attribute extraction For accurate vegetation comparison, the ICESat footprint shape and size needs to be accurately portrayed within the airborne LiDAR. Parameters for this have been extracted. Different lasers on satellite used over time – changes footprint shape
Selecting LiDAR in the ICESat footprint The ICESat data point is queried for the centre location coordinates, diameter, azimuth and shape (‘eccentricity’ = circle → ellipse) These parameters are input into an elliptical formula, where each LiDAR return is checked to see if it occurs within the footprint area
Extracting physical attributes from LiDAR A range of physical attributes were extracted from LiDAR data: • Slope – absolute ( from max – min elevation in footprint), and mean slope from 20 x 20m cells. • Mean elevation across footprint • Elevation range (max veg – min ground) • Max tree height (m) • Predominant tree height (m) across 10 x 10m cells • Foliage cover (% returns) @ 0.5 and 2 m height • Crown cover (%) (from crown delineation results)
Extracting Height Information 3 potential vegetation height parameters: centroid_height - distance from centre of ground pulse to centre of highest veg pulse fit_height - third parameter in the weibull distribution used to fit the cumulative vegetation profile - ( p[1] *exp (-p[2] * ( height x / p[3] )p[4] )) veg_height - Height where the cumulative FPC greater than 2m crosses 95%
Ground Elevation Comparisons – NE Victoria NE Victoria - mean elevation difference 1.67 m (stdev = 3.12 m, range –3.04 → 12.66 m) Many locations had ICESat with generally higher ground elevation, possibly due to: • denser canopies, • greater understorey presence, and • effect of slope in steeper terrain. • Definite ecozone / elevation trend
Those that recorded lower ICESat elevations were generally in riparian zones, where the 70-100m footprint could be influenced by terrain lower down river banks
Ground Elevation Comparisons –Qld
Injune - mean elevation difference was 0.16 m (sd = 1.31 m, range -2.0 → 2.73 m).
Close match to airborne lidar elevation possibly due to: • open canopies found in semi-arid environment, • generally flat terrain Indicates that ground elevation results may be good for most of Australia
Brisbane River mean elevation difference of 1.71 m (sd = 4.52 m, range -18.86 → 4.59 m).
ICESat value was mostly lower than LiDAR value,
Possibly larger footprint area recording range of elevation across stream bank slope, rather than at the footprint centre point higher up bank
The large 19 m difference observed at one site could be the result of the ICESat footprint overlapping a riverbank cliff
Ground Elevation Comparisons by Ecozone (NE Victoria)
Validation of ICESat attributes with LiDAR Best forest height comparisons were for max elevation range and predominant height
Crown and Foliage Cover comparisons rather poor
Quality Assessment for ICESat result by Ecozone Good = within 10% or 5m of LiDAR value, Poor = >20% or 10m of LiDAR Foliage cover Good – 33% Marg. – 26% Poor – 41%
Mean canopy height Good – 54% Marg. – 18% Poor – 28%
Vegetation Case Study
Vegetation Case Study Results
Vegetation Case Study Results Higher tree cover + lower slope = improved ICESat veg structure extraction
Midslope
Riparian Strip Ridgetop
ICESat Version 26 and 28 Version 26 – Aug 2006 Version 28 – Dec 2006 Version 26 • ~ 1.9 million footprints • FPC, 3 potential veg heights • Range of locations • Older processing algorithms
Version 28 • • • •
~ 2.6 million footprints Different FPC, 3 veg hts Less transects Newer algorithms, more consistently applied (older data reprocessed)
• 2008 update ~ 4 million footprints across Aust
Version 26 & 28 continental results Issues with Version 26 vs NFI data:
Version 26 continental summary
• Only 50% non-forest, (NFI ~ 80%) • Too much open forest (by ~ 30%) • Too much low forest (by ~25%)
Version 28 improvements: • Non forest within ~5% • All height classes within 5% wrt NFI • Open and closed forest within 6% • Woodland still underestimated
Version 28 continental summary
Enhanced national forest reporting NFI could report forest structure distributions as well as class summaries Provides improved assessment and monitoring of more subtle changes in height and cover Improved calibration of other remotely sensed data when using continuous, rather than categorical, data
Conclusions ICESat data has been successfully extracted Compared to airborne Lidar for 94 points at 3 main sites Strong agreement in ground elevation with airborne LiDAR Weaker but still reasonable relationship for forest height and cover in some cases: • Better for flatter terrain, with more open & shorter forests • Less reliable for taller dense forests on steeper terrain
Conclusions cont… Potential for forest vertical structure – but further calibration required for consistent extraction across environments Currently over ~4 million footprints across Australia, great sampling tool with preliminary results showing promise compared to existing NFI data National collaboration encouraged to share information • build a set of shared forest height and inventory data that can be used to calibrate, validate and develop modelling techniques