The 2014–2015 Lava Flow Field at Holuhraun, Iceland: Using Airborne Hyperspectral Remote Sensing for Discriminating the Lava Surface

The Holuhraun lava flow was the largest effusive eruption in Iceland for 230 years, with an estimated lava bulk volume of ~1.44 km 3 and covering an area of ~84 km 2 . The six month long eruption at Holuhraun 2014⁻2015 generated a diverse surface environment. Therefore, the abundant data of airborne...

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Bibliographic Details
Published in:Remote Sensing
Main Authors: Muhammad Aufaristama, Armann Hoskuldsson, Magnus Orn Ulfarsson, Ingibjorg Jonsdottir, Thorvaldur Thordarson
Format: Article in Journal/Newspaper
Language:English
Published: MDPI AG 2019
Subjects:
hyperspectral
FENIX
lava field
SMACC
LSMA
Science
Q
Holuhraun
Iceland
Online Access:https://doi.org/10.3390/rs11050476
https://doaj.org/article/62414ac32dc24a9baa779a279492dba5
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Summary:The Holuhraun lava flow was the largest effusive eruption in Iceland for 230 years, with an estimated lava bulk volume of ~1.44 km 3 and covering an area of ~84 km 2 . The six month long eruption at Holuhraun 2014⁻2015 generated a diverse surface environment. Therefore, the abundant data of airborne hyperspectral imagery above the lava field, calls for the use of time-efficient and accurate methods to unravel them. The hyperspectral data acquisition was acquired five months after the eruption finished, using an airborne FENIX-Hyperspectral sensor that was operated by the Natural Environment Research Council Airborne Research Facility (NERC-ARF). The data were atmospherically corrected using the Quick Atmospheric Correction (QUAC) algorithm. Here we used the Sequential Maximum Angle Convex Cone (SMACC) method to find spectral endmembers and their abundances throughout the airborne hyperspectral image. In total we estimated 15 endmembers, and we grouped these endmembers into six groups; (1) basalt; (2) hot material; (3) oxidized surface; (4) sulfate mineral; (5) water; and (6) noise. These groups were based on the similar shape of the endmembers; however, the amplitude varies due to illumination conditions, spectral variability, and topography. We, thus, obtained the respective abundances from each endmember group using fully constrained linear spectral mixture analysis (LSMA). The methods offer an optimum and a fast selection for volcanic products segregation. However, ground truth spectra are needed for further analysis.

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