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A comparison of airborne hyperspectral-based classifications of emergent wetland vegetation at Lake Balaton, Hungary

Version 2 2018-11-22, 15:14
Version 1 2018-09-12, 10:21
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posted on 2018-11-22, 15:14 authored by Dimitris Stratoulias, Heiko Balzter, András Zlinszky, Viktor R. Tóth

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 attributes. In this study, we investigate the capabilities of a concurrently acquired very high spatial resolution airborne hyperspectral and lidar data set at the peak of aquatic vegetation growth in a nature reserve at Lake Balaton, Hungary. The aim was to examine to what degree the different remote-sensing information sources (i.e. visible and near-infrared hyperspectral, vegetation indices and lidar) are contributing to an accurate aquatic vegetation map. The results indicate that de-noised hyperspectral information in the visible and very near-infrared bands (400–1000 nm) is performing most accurately. Inclusion of lidar information, hyperspectral infrared bands (1000–2500 nm), or extracted vegetation indices does not improve the classification accuracy. Experimental results with algorithmic comparisons show that in most cases, the Support Vector Machine classifier provides a better accuracy than the Maximum Likelihood.

Funding

This work was supported by GIONET, funded by the European Commission, Marie Curie Programme, Initial Training Networks under [Grant Agreement PITN-GA-2010-26450]. The airborne data were collected and provided by the Airborne Research and Survey Facility vested in the Natural Environment Research Council under the [EUFAR Contract Number 2271]. AZ was supported by the Hungarian Scientific Research Fund OTKA [grant PD 115833]. H. Balzter was supported by the Royal Society Wolfson Research Merit Award, 2011/R3 and the NERC National Centre for Earth Observation.

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