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Remote infrared detection of the cessation of volcanic eruptions
Author(s) -
Aries S. E.,
Harris A. J. L.,
Rothery D. A.
Publication year - 2001
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/2000gl012002
Subject(s) - radiance , volcano , geology , vulcanian eruption , lava , thermal infrared , effusive eruption , infrared , remote sensing , satellite , seismology , environmental science , astronomy , physics
When an effusive eruption ends lava surfaces initially cool rapidly so that within minutes temperatures across the hottest zones have dropped by 600°C. This means that eruption cessation is simple to detect using satellite infrared data, where a sudden, irrecoverable decline in thermal radiance, occurring over a period of hours, is characteristic of termination. AVHRR data acquired during and after 5 eruptions at Krafla (Iceland) illustrate this. In all cases the 3.9 µm spectral radiance in the first image following the known time of eruption cessation is markedly reduced compared to that recorded during the eruption, and subsequently remains at persistently low levels.