Evolution and future of the Lusi mud eruption inferred from ground deformation

The ongoing eruption of the Lusi mud volcano in East Java, Indonesia offers the unprecedented opportunity to study a large eruption from its beginning to its eventual end. We use new observations of ground deformation obtained from multitemporal interferometric analysis of L‐band synthetic aperture...

Full description

Saved in:
Bibliographic Details
Published in:Geophysical research letters 2013-03, Vol.40 (6), p.1089-1092
Main Authors: Rudolph, M. L., Shirzaei, M., Manga, M., Fukushima, Y.
Format: Article
Language:English
Subjects:
Decay rate
Deformation
Earth sciences
Earth, ocean, space
Evolution
Exact sciences and technology
Geophysics
Ground-based observation
Grounds
longevity
Lusi
Mud
Principal components analysis
Synthetic aperture radar
Volcanoes
Citations: Items that this one cites
Items that cite this one
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
Description
Summary:The ongoing eruption of the Lusi mud volcano in East Java, Indonesia offers the unprecedented opportunity to study a large eruption from its beginning to its eventual end. We use new observations of ground deformation obtained from multitemporal interferometric analysis of L‐band synthetic aperture radar data to show that Lusi will stop erupting much sooner than previously anticipated. Using principal component analysis, we find that the rate of ground deformation, and by implication, pressure in the mud source region, has been decaying exponentially with an e‐folding time scale of 2.1 ± 0.4 years. We anticipate that discharge will decrease to 10% of the present rate in 5 years. Key Points We measure ground deformation near Lusi using InSAR The rate of ground deformation is decreasing We anticipate that the eruption rate will decrease tenfold in 5 years
ISSN:0094-8276
1944-8007
DOI:10.1002/grl.50189