Synthetic aperture radar (SAR)-based mapping of volcanic flows: Manam Island, Papua New Guinea

We present new radar-based techniques for efficient identification of surface changes generated by lava and pyroclastic flows, and apply these to the 1996 eruption of Manam Volcano, Papua New Guinea. Polarimetric L- and P-band airborne synthetic aperture radar (SAR) data, along with a C-band DE...

Full description

Bibliographic Details
Main Authors: J. K. Weissel, K. R. Czuchlewski, Y. Kim
Format: Article
Language:English
Published: Copernicus Publications 2004-01-01
Series:Natural Hazards and Earth System Sciences
Online Access:http://www.nat-hazards-earth-syst-sci.net/4/339/2004/nhess-4-339-2004.pdf
id doaj-4645d5223adb40a1ae7b020ced209edd
record_format Article
spelling doaj-4645d5223adb40a1ae7b020ced209edd2020-11-24T22:34:16ZengCopernicus PublicationsNatural Hazards and Earth System Sciences1561-86331684-99812004-01-0142339346Synthetic aperture radar (SAR)-based mapping of volcanic flows: Manam Island, Papua New GuineaJ. K. WeisselK. R. CzuchlewskiK. R. CzuchlewskiY. KimWe present new radar-based techniques for efficient identification of surface changes generated by lava and pyroclastic flows, and apply these to the 1996 eruption of Manam Volcano, Papua New Guinea. Polarimetric L- and P-band airborne synthetic aperture radar (SAR) data, along with a C-band DEM, were acquired over the volcano on 17 November 1996 during a major eruption sequence. The L-band data are analyzed for dominant scattering mechanisms on a per pixel basis using radar target decomposition techniques. A classification method is presented, and when applied to the L-band polarimetry, it readily distinguishes bare surfaces from forest cover over Manam volcano. In particular, the classification scheme identifies a post-1992 lava flow in NE Valley of Manam Island as a mainly bare surface and the underlying 1992 flow units as mainly vegetated surfaces. The Smithsonian's Global Volcanism Network reports allow us to speculate whether the bare surface is a flow dating from October or November in the early part of the late-1996 eruption sequence. This work shows that fully polarimetric SAR is sensitive to scattering mechanism changes caused by volcanic resurfacing processes such as lava and pyroclastic flows. By extension, this technique should also prove useful in mapping debris flows, ash deposits and volcanic landslides associated with major eruptions.http://www.nat-hazards-earth-syst-sci.net/4/339/2004/nhess-4-339-2004.pdf
collection DOAJ
language English
format Article
sources DOAJ
author J. K. Weissel
K. R. Czuchlewski
K. R. Czuchlewski
Y. Kim
spellingShingle J. K. Weissel
K. R. Czuchlewski
K. R. Czuchlewski
Y. Kim
Synthetic aperture radar (SAR)-based mapping of volcanic flows: Manam Island, Papua New Guinea
Natural Hazards and Earth System Sciences
author_facet J. K. Weissel
K. R. Czuchlewski
K. R. Czuchlewski
Y. Kim
author_sort J. K. Weissel
title Synthetic aperture radar (SAR)-based mapping of volcanic flows: Manam Island, Papua New Guinea
title_short Synthetic aperture radar (SAR)-based mapping of volcanic flows: Manam Island, Papua New Guinea
title_full Synthetic aperture radar (SAR)-based mapping of volcanic flows: Manam Island, Papua New Guinea
title_fullStr Synthetic aperture radar (SAR)-based mapping of volcanic flows: Manam Island, Papua New Guinea
title_full_unstemmed Synthetic aperture radar (SAR)-based mapping of volcanic flows: Manam Island, Papua New Guinea
title_sort synthetic aperture radar (sar)-based mapping of volcanic flows: manam island, papua new guinea
publisher Copernicus Publications
series Natural Hazards and Earth System Sciences
issn 1561-8633
1684-9981
publishDate 2004-01-01
description We present new radar-based techniques for efficient identification of surface changes generated by lava and pyroclastic flows, and apply these to the 1996 eruption of Manam Volcano, Papua New Guinea. Polarimetric L- and P-band airborne synthetic aperture radar (SAR) data, along with a C-band DEM, were acquired over the volcano on 17 November 1996 during a major eruption sequence. The L-band data are analyzed for dominant scattering mechanisms on a per pixel basis using radar target decomposition techniques. A classification method is presented, and when applied to the L-band polarimetry, it readily distinguishes bare surfaces from forest cover over Manam volcano. In particular, the classification scheme identifies a post-1992 lava flow in NE Valley of Manam Island as a mainly bare surface and the underlying 1992 flow units as mainly vegetated surfaces. The Smithsonian's Global Volcanism Network reports allow us to speculate whether the bare surface is a flow dating from October or November in the early part of the late-1996 eruption sequence. This work shows that fully polarimetric SAR is sensitive to scattering mechanism changes caused by volcanic resurfacing processes such as lava and pyroclastic flows. By extension, this technique should also prove useful in mapping debris flows, ash deposits and volcanic landslides associated with major eruptions.
url http://www.nat-hazards-earth-syst-sci.net/4/339/2004/nhess-4-339-2004.pdf
work_keys_str_mv AT jkweissel syntheticapertureradarsarbasedmappingofvolcanicflowsmanamislandpapuanewguinea
AT krczuchlewski syntheticapertureradarsarbasedmappingofvolcanicflowsmanamislandpapuanewguinea
AT krczuchlewski syntheticapertureradarsarbasedmappingofvolcanicflowsmanamislandpapuanewguinea
AT ykim syntheticapertureradarsarbasedmappingofvolcanicflowsmanamislandpapuanewguinea
_version_ 1725728526310572032