2010
DOI: 10.1109/tgrs.2010.2040831
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ICESat Geolocation Validation Using Airborne Photography

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Cited by 23 publications
(8 citation statements)
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“…There are several main methods of space-borne laser altimeter calibration: verification with high-resolution and precise airborne laser altimeter data and other elevation data [ 10 ]; systematic pointing error calibration with ocean and round-the-world scan crossovers using aerial photography to assist the space-borne laser altimeter calibration [ 17 ]; and high-precision onboard geometric calibration based on a land infrared detector array [ 11 , 18 ].…”
Section: Basic Informationmentioning
confidence: 99%
See 1 more Smart Citation
“…There are several main methods of space-borne laser altimeter calibration: verification with high-resolution and precise airborne laser altimeter data and other elevation data [ 10 ]; systematic pointing error calibration with ocean and round-the-world scan crossovers using aerial photography to assist the space-borne laser altimeter calibration [ 17 ]; and high-precision onboard geometric calibration based on a land infrared detector array [ 11 , 18 ].…”
Section: Basic Informationmentioning
confidence: 99%
“…The idea of calibration test is simple in concept, but there are some difficulties in the process, such as how to determine the size and geolocation of the electro-optical detector array. The laser emitting frequency of GLAS is 40 Hz, which can result in a spatial distance between along-track neighboring footprint centers where the distance is 172 m. We can capture no fewer than one footprint if the size of an along-track array is larger than 172 m and the cross-track is larger than 100 m [ 16 , 17 , 18 , 19 ].…”
Section: Introductionmentioning
confidence: 99%
“…One deploys laser detectors and the other involves waveform matching between the laser echo simulated by a high-precision digital surface model (DSM) and the actual laser echo. Some studies have attempted to address this issue by arranging infrared signal detectors on the ground surface [16][17][18][19]. Others have used the unique signal generated in the reflected wave by the corner cube retroreflector (CCR) to obtain time information for calibrating synchronization errors [20,21].…”
Section: Introductionmentioning
confidence: 99%
“…Magruder et al. (, ) used a unique signal that was caused by a reflected waveform from corner‐cube retroreflectors to calibrate a time synchronisation error. Martin et al.…”
Section: Introductionmentioning
confidence: 99%