Abstract
Satellite-based estimates of vegetation structure capture broad-scale vegetation characteristics as well as differences in vegetation structure at plot-scales. Active remote sensing from laser altimetry and radar systems is regularly used to measure vegetation height and infer vegetation structural attributes, however, the current uncertainty of their spaceborne measurements is likely to mask actual plot-scale differences in vertical structures in sparse forests. In the taiga (boreal forest)—tundra ecotone (TTE) the accumulated effect of subtle plot-scale differences in vegetation height across broad-scales may be significant. This paper examines the uncertainty of plot-scale forest canopy height measurements in northern Siberia Larix stands by combining complementary canopy surface elevations derived from satellite photogrammetry and ground elevations derived from the Geosciences Laser Altimeter System (GLAS) from the ICESat-1 satellite. With a linear model, spaceborne-derived canopy height measurements at the plot-scale predicted TTE stand height ~5 m–~10 m tall (R2 = 0.55, bootstrapped 95% confidence interval of R2 = 0.36–0.74) with an uncertainty ranging from ±0.86 m–1.37 m. A larger sample may mitigate the broad uncertainty of the model fit, however, the methodology provides a means for capturing plot-scale canopy height and its uncertainty from spaceborne data at GLAS footprints in sparse TTE forests and may serve as a basis for scaling up plot-level TTE vegetation height measurements to forest patches.
Highlights
Boreal vegetation structure is an important factor in the arctic climate system [1,2]
The objective of this paper is to evaluate the uncertainty of canopy height estimates from complementary spaceborne measurements in the tundra ecotone (TTE)
Spaceborne forest canopy height estimates were calculated as the difference of ground surface elevations measurements and canopy surface elevation measurements at field plots centered on Geosciences Laser Altimeter System (GLAS) footprints in forest stands
Summary
Boreal vegetation structure is an important factor in the arctic climate system [1,2]. The taiga-tundra ecotone (TTE) at the convergence of the boreal forest and un-forested tundra has heterogeneous tree cover, and has seen recent widespread, yet variable, changes in vegetation structure [3,4,5,6,7]. Vegetation structural attributes, such as height, may influence ground temperatures, active-layer depth, albedo, and atmospheric warming [8,9,10,11,12,13,14]. The synoptic yet detailed perspective of plot-level vegetation characteristics and spatial arrangement derived from high-resolution (
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