2018
DOI: 10.1080/01431161.2018.1466081
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A comparison of airborne hyperspectral-based classifications of emergent wetland vegetation at Lake Balaton, Hungary

Abstract: Earth observation has rapidly evolved into a state-of-the-art technology providing new capabilities and a wide variety of sensors; nevertheless, it is still a challenge for practitioners external to a specialized community of experts to select the appropriate sensor, define the imaging mode requirements, and select the optimal classifier or retrieval method for the task at hand. Especially in wetland mapping, studies have relied largely on vegetation indices and hyperspectral data to capture vegetation attribu… Show more

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Cited by 21 publications
(13 citation statements)
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“…The steep windward northern shore's sediment consists of dolomite limestone, while the shallow southern shore is dominated by sandy sediment. On the northern shore of the lake the average and maximum depth of water that reed stand can be found is 1.5 m and 2.4 m respectively, while on the southern shore the average depth on the waterward side of reed stands is 1 m [40,41] Lake Balaton has received significant scientific attention due to the reed die-back phenomenon observed (e.g., [40][41][42][43]), the macrophytic traits and species mapping (e.g., [44][45][46][47]) and the dynamic trophic gradient of the water (e.g., [48,49]). The field data for this study were collected at the Kerekedi bay, an oligo-mesotrophic bay at the easternmost basin of Lake Balaton situated at the geographic coordinates 46 • Map of the study area in Lake Balaton (inset) and field sampling points' location in the Kerekedi Bay (main).…”
Section: Study Sitementioning
confidence: 99%
“…The steep windward northern shore's sediment consists of dolomite limestone, while the shallow southern shore is dominated by sandy sediment. On the northern shore of the lake the average and maximum depth of water that reed stand can be found is 1.5 m and 2.4 m respectively, while on the southern shore the average depth on the waterward side of reed stands is 1 m [40,41] Lake Balaton has received significant scientific attention due to the reed die-back phenomenon observed (e.g., [40][41][42][43]), the macrophytic traits and species mapping (e.g., [44][45][46][47]) and the dynamic trophic gradient of the water (e.g., [48,49]). The field data for this study were collected at the Kerekedi bay, an oligo-mesotrophic bay at the easternmost basin of Lake Balaton situated at the geographic coordinates 46 • Map of the study area in Lake Balaton (inset) and field sampling points' location in the Kerekedi Bay (main).…”
Section: Study Sitementioning
confidence: 99%
“…However, pixel-based classification performance is always limited for complicated landscape with diverse landcover types and their small patch sizes [40]. Moreover, spectral variations cause different species to have similar spectral signatures [41]. Single source of spectral information may not distinguish mixed species composition of wetlands and often leads to low mapping accuracies.…”
Section: Introductionmentioning
confidence: 99%
“…However, there is much more to anticipate from this historic archive; the 0.5-0.9μm spectral domain of the panchromatic layer has been shown to be the most important spectral region for vegetation-related studies (e.g. [14][15][16][17]) and the very high spatial resolution is suitable for small agricultural field parcels delineation [18][19] (if not necessary [20]) which appears to be the norm in Bulgaria of the 1960s.…”
Section: Introductionmentioning
confidence: 99%