GOES satellite and field observations of the 1998 eruption of Volcan CerroAzul, Galapagos Islands

Citation
Pj. Mouginis-mark et al., GOES satellite and field observations of the 1998 eruption of Volcan CerroAzul, Galapagos Islands, B VOLCANOL, 62(3), 2000, pp. 188-198
Citations number
10
Categorie Soggetti
Earth Sciences
Journal title
BULLETIN OF VOLCANOLOGY
ISSN journal
02588900 → ACNP
Volume
62
Issue
3
Year of publication
2000
Pages
188 - 198
Database
ISI
SICI code
0258-8900(200008)62:3<188:GSAFOO>2.0.ZU;2-Y
Abstract
The 1998 eruption of Volcan Cerro Azul, Isla Isabela, Galapagos Islands, wa s observed in near real-time by the Geostationary Operational Environmental Satellite-8 (GOES-8) weather satellite. Due to the remote location of the eruption site, 3.9-mu m radiance values derived from GOES band 2 provide th e best timing of the start and termination of the eruption, which occurred on 15 Sept. and 21 Oct., respectively. Throughout the 36-day long eruption, a total of 1335 thermal infrared images were collected, of which 851 were cloud-free and permitted the thermal anomaly to be detected. A detailed chr onology including 77 separate events was assembled from the GOES data and f ield observations. Numerous attributes of the eruption were observed from t he GOES data, including the sizes and dispersal of seven eruption plumes an d the occurrence and timing of intra-caldera effusive activity. The growth of a lava flow on the SE flank, the formation of smoke and volcanic haze fr om the flank vent, and burning of vegetation caused by lava flows entering vegetated areas were monitored both on the ground and with the satellite da ta. In most cases GOES images were processed as they were received every 30 min and were then distributed over the Internet within minutes of receptio n. These data provided timely high-temporal information to field parties as well as enabled the documentation of the eruption. The GOES observations o f Cerro Azul serve as a further example of the way in which the remote sens ing community and field volcanologists can collaborate during future: erupt ions, and permit the temporal and spatial resolution requirements for futur e satellites systems to be better defined.