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Linking hydrological connectivity to gully erosion in savanna rangelands tributary to the Great Barrier Reef using Structure‐from‐Motion photogrammetry
Journal article   Open access   Peer reviewed

Linking hydrological connectivity to gully erosion in savanna rangelands tributary to the Great Barrier Reef using Structure‐from‐Motion photogrammetry

Jack Koci, Roy C Sidle, Ben Jarihani and Matthew J Cashman
Land Degradation & Development, Vol.31(1), pp.20-36
2020
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Linking hydrological connectivity to gully erosion in savanna rangelands tributary to the Great Barrier Reef using Structure‐from‐Motion photogrammetry5.41 MBDownloadView
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https://doi.org/10.1002/ldr.3421View
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Abstract

drone hydrogeomorphology index of connectivity overland flow runoff Unmanned Aircraft System (UAS)
Gully erosion is a major land management challenge globally and a particularly significant issue in dry-tropical savanna rangelands tributary to the Great Barrier Reef, Australia. This study investigated linkages between hillslope hydrological connectivity pathways and gully geomorphic change in the Burdekin River basin. High resolution (0.1 m) topographic and land cover data derived from low-cost aerial (via Unmanned Aircraft System, UAS) structure-from-motion with multi-view stereo photogrammetry (SfM) was used to map fine-scale connectivity patterns and quantify headcut retreat at the hillslope scale (~150,000 m2). Very high resolution (0.01 m) topographic models derived from ground-based (via hand-held digital camera, GB) SfM, were used to quantify the morphology and geomorphic change of several gully arms (300-700 m2) between 2016 and 2018. Median linear, areal, and volumetric headcut (n=21) retreat rates were 0.2 m yr-1, 0.8 m2 yr-1, and 0.3 m3 yr-1, respectively. At all study sites, the points where modelled hydrological flow lines intersected gullies corresponded to observed geomorphic change, enabling spatially explicit identification of gully extension pathways as a result of overland flow. Application of an index of connectivity demarcated parts of the hillslope most connected to the gully network. Bare areas, roads and cattle trails were identified as important runoff source areas and hydrological conduits driving gully extension. GB SfM accurately reconstructed complex morphologic features including undercuts, overhangs, rills and flutes, providing insights into within-channel erosion processes. This study contributes to an improved understanding and modelling of hydrogeomorphic drivers of gully erosion in degraded savanna rangelands, ultimately benefiting gully management.

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Environmental Sciences
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