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Assessment of terrain elevation derived from satellite laser altimetry over mountainous forest areas using airborne lidar data
Authors:Qi Chen
Affiliation:1. LiDAR Applications for the Study of Ecosystems with Remote Sensing (LASERS) Laboratory, Department of Ecosystem Science and Management, Texas A &M University, College Station, TX 77450, USA;2. Biospheric Sciences Lab, Code 618, NASA-GSFC, Greenbelt, MD 20771, USA;3. Geospatial Laser Applications and Measurements, Applied Research Laboratories, University of Texas at Austin, 10000 Burnet Rd, Austin, TX 78758, USA;4. NASA Goddard Space Flight Center, Greenbelt, MD 20771, USA;1. Global Environmental Modelling and Earth Observation (GEMEO), Department of Geography, Swansea University, SA2 8PP, United Kingdom;2. Department of Geography, University of Lethbridge, 4401 University Drive, Lethbridge, Alberta T1K 3M4, Canada
Abstract:Gaussian decomposition has been used to extract terrain elevation from waveforms of the satellite lidar GLAS (Geoscience Laser Altimeter System), on board ICESat (Ice, Cloud, and land Elevation Satellite). The common assumption is that one of the extracted Gaussian peaks, especially the lowest one, corresponds to the ground. However, Gaussian decomposition is usually complicated due to the broadened signals from both terrain and objects above over sloped areas. It is a critical and pressing research issue to quantify and understand the correspondence between Gaussian peaks and ground elevation. This study uses ~2000 km2 airborne lidar data to assess the lowest two GLAS Gaussian peaks for terrain elevation estimation over mountainous forest areas in North Carolina. Airborne lidar data were used to extract not only ground elevation, but also terrain and canopy features such as slope and canopy height. Based on the analysis of a total of ~500 GLAS shots, it was found that (1) the lowest peak tends to underestimate ground elevation; terrain steepness (slope) and canopy height have the highest correlation with the underestimation, (2) the second to the lowest peak is, on average, closer to the ground elevation over mountainous forest areas, and (3) the stronger peak among the lowest two is closest to the ground for both open terrain and mountainous forest areas. It is expected that this assessment will shed light on future algorithm improvements and/or better use of the GLAS products for terrain elevation estimation.
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