High Resolution Aircraft Scanner Mapping of Geothermal and Volcanic Areas

High spectral resolution GEOSCAN Mkll multispectral aircraft scanner imagery has been acquired, at 3-6 m spatial resolutions, over much of the Taupo Volcanic Zone as part of continuing investigations aimed at developing remote sensing techniques for exploring and mapping geothermal and volcanic area...

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Main Authors: Mongillo, M.A., Cochrane, G.R., Wood, C.P., Shibata, Y.
Language:unknown
Published: 2007
Subjects:
Online Access:http://www.osti.gov/servlets/purl/895889
https://www.osti.gov/biblio/895889
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spelling ftosti:oai:osti.gov:895889 2023-07-30T04:07:25+02:00 High Resolution Aircraft Scanner Mapping of Geothermal and Volcanic Areas Mongillo, M.A. Cochrane, G.R. Wood, C.P. Shibata, Y. 2007-03-05 application/pdf http://www.osti.gov/servlets/purl/895889 https://www.osti.gov/biblio/895889 unknown http://www.osti.gov/servlets/purl/895889 https://www.osti.gov/biblio/895889 15 GEOTHERMAL ENERGY AIRCRAFT COLOR GEOTHERMAL FIELDS HYDROTHERMAL ALTERATION ISLANDS NEW ZEALAND PLANTS REMOTE SENSING RESOLUTION SPATIAL RESOLUTION WATER WAVELENGTHS 2007 ftosti 2023-07-11T08:44:09Z High spectral resolution GEOSCAN Mkll multispectral aircraft scanner imagery has been acquired, at 3-6 m spatial resolutions, over much of the Taupo Volcanic Zone as part of continuing investigations aimed at developing remote sensing techniques for exploring and mapping geothermal and volcanic areas. This study examined the 24-band: visible, near-IR (NIR), mid-IR (MIR) and thermal-IR (TIR) imagery acquired over Waiotapu geothermal area (3 m spatial resolution) and White Island volcano (6 m resolution). Results show that color composite images composed of visible and NIR wavelengths that correspond to color infrared (CIR) photographic wavelengths can be useful for distinguishing among bare ground, water and vegetation features and, in certain cases, for mapping various vegetation types. However, combinations which include an MIR band ({approx} 2.2 {micro}m) with either visible and NIR bands, or two NIR bands, are the most powerful for mapping vegetation types, water bodies, and bare and hydrothermally altered ground. Combinations incorporating a daytime TIR band with NIR and MIR bands are also valuable for locating anomalously hot features and distinguishing among different types of surface hydrothermal alteration. Other/Unknown Material White Island SciTec Connect (Office of Scientific and Technical Information - OSTI, U.S. Department of Energy) New Zealand White Island ENVELOPE(48.583,48.583,-66.733,-66.733)
institution Open Polar
collection SciTec Connect (Office of Scientific and Technical Information - OSTI, U.S. Department of Energy)
op_collection_id ftosti
language unknown
topic 15 GEOTHERMAL ENERGY
AIRCRAFT
COLOR
GEOTHERMAL FIELDS
HYDROTHERMAL ALTERATION
ISLANDS
NEW ZEALAND
PLANTS
REMOTE SENSING
RESOLUTION
SPATIAL RESOLUTION
WATER
WAVELENGTHS
spellingShingle 15 GEOTHERMAL ENERGY
AIRCRAFT
COLOR
GEOTHERMAL FIELDS
HYDROTHERMAL ALTERATION
ISLANDS
NEW ZEALAND
PLANTS
REMOTE SENSING
RESOLUTION
SPATIAL RESOLUTION
WATER
WAVELENGTHS
Mongillo, M.A.
Cochrane, G.R.
Wood, C.P.
Shibata, Y.
High Resolution Aircraft Scanner Mapping of Geothermal and Volcanic Areas
topic_facet 15 GEOTHERMAL ENERGY
AIRCRAFT
COLOR
GEOTHERMAL FIELDS
HYDROTHERMAL ALTERATION
ISLANDS
NEW ZEALAND
PLANTS
REMOTE SENSING
RESOLUTION
SPATIAL RESOLUTION
WATER
WAVELENGTHS
description High spectral resolution GEOSCAN Mkll multispectral aircraft scanner imagery has been acquired, at 3-6 m spatial resolutions, over much of the Taupo Volcanic Zone as part of continuing investigations aimed at developing remote sensing techniques for exploring and mapping geothermal and volcanic areas. This study examined the 24-band: visible, near-IR (NIR), mid-IR (MIR) and thermal-IR (TIR) imagery acquired over Waiotapu geothermal area (3 m spatial resolution) and White Island volcano (6 m resolution). Results show that color composite images composed of visible and NIR wavelengths that correspond to color infrared (CIR) photographic wavelengths can be useful for distinguishing among bare ground, water and vegetation features and, in certain cases, for mapping various vegetation types. However, combinations which include an MIR band ({approx} 2.2 {micro}m) with either visible and NIR bands, or two NIR bands, are the most powerful for mapping vegetation types, water bodies, and bare and hydrothermally altered ground. Combinations incorporating a daytime TIR band with NIR and MIR bands are also valuable for locating anomalously hot features and distinguishing among different types of surface hydrothermal alteration.
author Mongillo, M.A.
Cochrane, G.R.
Wood, C.P.
Shibata, Y.
author_facet Mongillo, M.A.
Cochrane, G.R.
Wood, C.P.
Shibata, Y.
author_sort Mongillo, M.A.
title High Resolution Aircraft Scanner Mapping of Geothermal and Volcanic Areas
title_short High Resolution Aircraft Scanner Mapping of Geothermal and Volcanic Areas
title_full High Resolution Aircraft Scanner Mapping of Geothermal and Volcanic Areas
title_fullStr High Resolution Aircraft Scanner Mapping of Geothermal and Volcanic Areas
title_full_unstemmed High Resolution Aircraft Scanner Mapping of Geothermal and Volcanic Areas
title_sort high resolution aircraft scanner mapping of geothermal and volcanic areas
publishDate 2007
url http://www.osti.gov/servlets/purl/895889
https://www.osti.gov/biblio/895889
long_lat ENVELOPE(48.583,48.583,-66.733,-66.733)
geographic New Zealand
White Island
geographic_facet New Zealand
White Island
genre White Island
genre_facet White Island
op_relation http://www.osti.gov/servlets/purl/895889
https://www.osti.gov/biblio/895889
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