Improved identification of volcanic features using Landsat 7 ETM+

Citation
Lp. Flynn et al., Improved identification of volcanic features using Landsat 7 ETM+, REMOT SEN E, 78(1-2), 2001, pp. 180-193
Citations number
52
Categorie Soggetti
Earth Sciences
Journal title
REMOTE SENSING OF ENVIRONMENT
ISSN journal
00344257 → ACNP
Volume
78
Issue
1-2
Year of publication
2001
Pages
180 - 193
Database
ISI
SICI code
0034-4257(200110)78:1-2<180:IIOVFU>2.0.ZU;2-U
Abstract
Volcanic eruptions can present unpredictable hazards to populations living within regions containing potentially active volcanoes and for people trave ling in jet aircraft that intersect with ash-laden eruption clouds. Methods of monitoring volcanic activity include searching for variations in the th ermal signal from active fumaroles, lava domes, lava lakes, flows, and othe r features. Over many active volcanoes in the Western Hemisphere, low spati al resolution (4 km/pixel) weather satellite data acquired every 15 min are used to identify changes in eruptive activity, but are of insufficient spa tial resolution to map active volcanic features. The Enhanced Thematic Mapp er Plus (ETM+) on Landsat 7 can be used to monitor active volcanoes at a hi gher spatial resolution (15- to 60-m pixels). ETM+ also offers improvements over its predecessor, the Thematic Mapper of Landsats 4 and 5, by way of a 15-m panchromatic band and higher spatial resolution (60 m/pixel) thermal infrared (IR) band. With higher spatial resolution panchromatic data, we ar e able to map lava flow fields, trace very high temperature lava channels, and, at Lascar volcano, identify an arcuate feature associated with a colla psed crater floor, a phenomenon that may precede explosive activity. With i mproved spatial resolution in the thermal IR, we are able to map the bifurc ation and braiding of underground lava tubes at Kilauea. Identifying tube l ocations and tracking their extension are important because, for a given vo lumetric lava production (effusion) rate, tube-fed flows can extend a much greater distance than surface flows. At both Kilauea and Etna, we are able to use the thermal data to estimate effusion rates, an important parameter for assessing how far a flow is likely to extend and therefore the hazard i t poses. An improved ETM+ data collection and distribution system includes a well-formulated and -executed Long-Term Acquisition Plan and less expensi ve data that is available much faster than previously possible. (C) 2001 El sevier Science Inc. All rights reserved.