The impact of geolocation uncertainty on GEDI tropical forest canopy height estimation and change monitoring

被引:84
作者
Roy, David P. [1 ,2 ,4 ]
Kashongwe, Herve B. [2 ]
Armston, John [3 ]
机构
[1] Michigan State Univ, Ctr Global Change & Earth Observat, E Lansing, MI USA
[2] Michigan State Univ, Dept Geog Environmeny & Spatial Sci, E Lansing, MI USA
[3] Univ Maryland, Dept Geog Sci, College Pk, MD USA
[4] Michigan State Univ, E Lansing, MI 48824 USA
来源
SCIENCE OF REMOTE SENSING | 2021年 / 4卷
关键词
GEDI; Forest; Change; Geolocation; Airborne; LiDAR; Simulation; PlanetScope; MULTITEMPORAL LIDAR; WAVE-FORMS; BIOMASS; MISREGISTRATION; COVER; GEOSTATISTICS; ACCURACY; AFRICAN; GROWTH; SIZE;
D O I
10.1016/j.srs.2021.100024
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The Global Ecosystem Dynamics Investigation (GEDI) LiDAR provides new spaceborne vegetation canopy structural information including relative canopy height products defined with respect to 25 m diameter foot-prints. The GEDI geolocation requirement is that each 25 m footprint center is horizontally georeferenced to within 10 m (1 & sigma;), assuming normally distributed geolocation errors with a 0 m mean and a 10 m standard deviation. The impact of this geolocation uncertainty on the reliability of forest canopy height estimation is examined considering Airborne Laser scanner (ALS) and GEDI data acquired in 2014 and 2019 respectively. A total of 445 GEDI footprints acquired over 2000 ha of unforested and tropical secondary forest in the western Democratic Republic of the Congo with vegetation heights ranging from 1 m to 42 m are considered. Airborne true color 10 cm imagery and an ALS derived canopy height model are examined to contextualize the results. GEDI waveforms are simulated from the ALS data at the reported locations of the GEDI footprints and used to derive h95, h85, h75relative heights that define the canopy height relative to the ground below which 95%, 85% and 75% of the simulated cumulative waveform energy is returned. A Monte Carlo simulation is undertaken, moving the centers of each GEDI footprint with 300 randomly generated position errors modelled using the GEDI geolocation uncertainty (0 m mean, 10 m standard deviation), and each time simulating the GEDI waveform from the ALS data. Relative heights are extracted from the 300 simulated GEDI waveforms and their variation, defined by the 25th and 75th percentiles, and the interquartile range (IQR) (75th -25th percentiles), are quantified to provide insights into the impact of the GEDI geolocation uncertainty on forest canopy height retrieval. The IQR accounts for 50% of the variation in the forest canopy height due to GEDI geolocation un-certainty. High IQR values, greater than or comparable to the relative height derived from the ALS data at the GEDI reported footprint location are shown to occur where the footprint covered or was adjacent to spatially heterogeneous canopies, including canopies with small forest stands, holes in the vegetation canopy, and forest edges. This is a concern for the use of GEDI data acquired over these conditions which are prevalent in many forest systems. The impact of GEDI geolocation uncertainty on tropical forest change monitoring is demonstrated by comparing the GEDI h95 product footprint values (sensed in 2019) with simulated h95 values derived from the ALS data (sensed in 2014) at the GEDI product reported footprint location and at the 300 shifted footprint lo-cations. GEDI footprints where five-year canopy height changes, and not changes due to artefacts associated with the GEDI geolocation uncertainty or the GEDI simulator, are attributed conservatively. Differences among the six algorithm setting group GEDI h95 product relative height values are evident and influential on the change attribution. PlanetScope 3 m imagery sensed in 2019 are examined to provide qualitative evidence that support the efficacy of the approach for forest height reduction monitoring. The simulation approach described in this study provides a route to determine if forest canopy height change found by comparing multi-temporal data (for example, GEDI with previously collected ALS data or GEDI data) is significant relative to errors imposed by the GEDI geolocation. The treatment of change is simple, and recommendations for improvements to detect more subtle change are made. The study was undertaken using the Release 1.0 GEDI data and suggests, pending planned geolocation improvement, the need to accommodate for GEDI geolocation uncertainty, particularly over canopies that are spatially fragmented or that have heterogeneous three dimensional structure at scales com-parable to the 25 m GEDI footprint dimension.
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页数:19
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共 77 条
  • [1] Global hydroclimatological teleconnections resulting from tropical deforestation
    Avissar, R
    Werth, D
    [J]. JOURNAL OF HYDROMETEOROLOGY, 2005, 6 (02) : 134 - 145
  • [2] Beck J., 2021, Global Ecosystem dynamics investigation (GEDI) level 02 user guide. Document version 2.0
  • [3] Beck J., 2020, Global Ecosystem Dynamics Investigation
  • [4] Modeling laser altimeter return waveforms over complex vegetation using high-resolution elevation data
    Blair, JB
    Hofton, MA
    [J]. GEOPHYSICAL RESEARCH LETTERS, 1999, 26 (16) : 2509 - 2512
  • [5] Detecting Change in Forest Structure with Simulated GEDI Lidar Waveforms: A Case Study of the Hemlock Woolly Adelgid (HWA; Adelges tsugae) Infestation
    Boucher, Peter Brehm
    Hancock, Steven
    Orwig, David A.
    Duncanson, Laura
    Armston, John
    Tang, Hao
    Krause, Keith
    Cook, Bruce
    Paynter, Ian
    Li, Zhan
    Elmes, Arthur
    Schaaf, Crystal
    [J]. REMOTE SENSING, 2020, 12 (08)
  • [6] Toward an integrated monitoring framework to assess the effects of tropical forest degradation and recovery on carbon stocks and biodiversity
    Bustamante, Mercedes M. C.
    Roitman, Iris
    Aide, T. . Mitchell
    Alencar, Ane
    Anderson, Liana O.
    Aragao, Luiz
    Asner, Gregory P.
    Barlow, Jos
    Berenguer, Erika
    Chambers, Jeffrey
    Costa, Marcos H.
    Fanin, Thierry
    Ferreira, Laerte G.
    Ferreira, Joice
    Keller, Michael
    Magnusson, William E.
    Morales-Barquero, Lucia
    Morton, Douglas
    Ometto, Jean P. H. B.
    Palace, Michael
    Peres, Carlos A.
    Silverio, Divino
    Trumbore, Susan
    Vieira, Ima C. G.
    [J]. GLOBAL CHANGE BIOLOGY, 2016, 22 (01) : 92 - 109
  • [7] Identifying nascent wetland forest conversion in the Democratic Republic of the Congo
    Bwangoy, Jean-Robert B.
    Hansen, Matthew C.
    Potapov, Peter
    Turubanova, Svetlana
    Lumbuenamo, Raymond S.
    [J]. WETLANDS ECOLOGY AND MANAGEMENT, 2013, 21 (01) : 29 - 43
  • [8] Wetland mapping in the Congo Basin using optical and radar remotely sensed data and derived topographical indices
    Bwangoy, Jean-Robert B.
    Hansen, Matthew C.
    Roy, David P.
    De Grandi, Gianfranco
    Justice, Christopher O.
    [J]. REMOTE SENSING OF ENVIRONMENT, 2010, 114 (01) : 73 - 86
  • [9] Terrestrial laser scanning in forest ecology: Expanding the horizon
    Calders, Kim
    Adams, Jennifer
    Armston, John
    Bartholomeus, Harm
    Bauwens, Sebastien
    Bentley, Lisa Patrick
    Chave, Jerome
    Danson, F. Mark
    Demol, Miro
    Disney, Mathias
    Gaulton, Rachel
    Moorthy, Sruthi M. Krishna
    Levick, Shaun R.
    Saarinen, Ninni
    Schaaf, Crystal
    Stovall, Atticus
    Terryn, Louise
    Wilkes, Phil
    Verbeeck, Hans
    [J]. REMOTE SENSING OF ENVIRONMENT, 2020, 251
  • [10] Recovery and resilience of tropical forests after disturbance
    Cole, Lydia E. S.
    Bhagwat, Shonil A.
    Willis, Katherine J.
    [J]. NATURE COMMUNICATIONS, 2014, 5