Publications
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Interferometric synthetic aperture radar (InSAR)—its past, present and future Interferometric synthetic aperture radar (InSAR)—its past, present and future
Very simply, interferometric synthetic aperture radar (InSAR) involves the use of two or more synthetic aperture radar (SAR) images of the same area to extract landscape topography and its deformation patterns. A SAR system transmits electromagnetic waves at a wavelength that can range from a few millimeters to tens of centimeters and therefore can operate during day and night under all...
Authors
Zhong Lu, Oh-Ig Kwoun, R.P. Rykhus
InSAR imaging of volcanic deformation over cloud-prone areas - Aleutian islands InSAR imaging of volcanic deformation over cloud-prone areas - Aleutian islands
Interferometric synthetic aperture radar (INSAR) is capable of measuring ground-surface deformation with centimeter-tosubcentimeter precision and spatial resolution of tens-of meters over a relatively large region. With its global coverage and all-weather imaging capability, INSAR is an important technique for measuring ground-surface deformation of volcanoes over cloud-prone and rainy...
Authors
Zhong Lu
Electrical activity during the 2006 Mount St. Augustine volcanic eruptions Electrical activity during the 2006 Mount St. Augustine volcanic eruptions
By using a combination of radio frequency time-of-arrival and interferometer measurements, we observed a sequence of lightning and electrical activity during one of Mount St. Augustine's eruptions. The observations indicate that the electrical activity had two modes or phases. First, there was an explosive phase in which the ejecta from the explosion appeared to be highly charged upon...
Authors
Ronald J. Thomas, Paul R. Krehbiel, William Rison, H. E. Edens, G. D. Aulich, S.R. McNutt, Guy Tytgat, E. Clark
Volcanic ash plume identification using polarization lidar: Augustine eruption, Alaska Volcanic ash plume identification using polarization lidar: Augustine eruption, Alaska
During mid January to early February 2006, a series of explosive eruptions occurred at the Augustine volcanic island off the southern coast of Alaska. By early February a plume of volcanic ash was transported northward into the interior of Alaska. Satellite imagery and Puff volcanic ash transport model predictions confirm that the aerosol plume passed over a polarization lidar (0.694 mm...
Authors
Kenneth Sassen, Jiang Zhu, Peter W. Webley, K. Dean, Patrick Cobb
Modeling the dynamic response of a crater glacier to lava-dome emplacement: Mount St Helens, Washington, USA Modeling the dynamic response of a crater glacier to lava-dome emplacement: Mount St Helens, Washington, USA
The debris-rich glacier that grew in the crater of Mount St Helens after the volcano's cataclysmic 1980 eruption was split in two by a new lava dome in 2004. For nearly six months, the eastern part of the glacier was squeezed against the crater wall as the lava dome expanded. Glacier thickness nearly doubled locally and surface speed increased substantially. As squeezing slowed and then...
Authors
Stephen F. Price, Joseph S. Walder
Crisis GIS--Preparing for and responding to volcanic eruptions in the United States Crisis GIS--Preparing for and responding to volcanic eruptions in the United States
No abstract available.
Authors
D.W. Ramsey, J.E. Robinson, S. P. Schilling, J.R. Schaefer, Frank A. Trusdell
A user-friendly one-dimensional model for wet volcanic plumes A user-friendly one-dimensional model for wet volcanic plumes
This paper presents a user-friendly graphically based numerical model of one-dimensional steady state homogeneous volcanic plumes that calculates and plots profiles of upward velocity, plume density, radius, temperature, and other parameters as a function of height. The model considers effects of water condensation and ice formation on plume dynamics as well as the effect of water added...
Authors
Larry G. Mastin
Hydrothermal systems and volcano geochemistry Hydrothermal systems and volcano geochemistry
The upward intrusion of magma from deeper to shallower levels beneath volcanoes obviously plays an important role in their surface deformation. This chapter will examine less obvious roles that hydrothermal processes might play in volcanic deformation. Emphasis will be placed on the effect that the transition from brittle to plastic behavior of rocks is likely to have on magma degassing...
Authors
R.O. Fournier
Strombolian explosive styles and source conditions Strombolian explosive styles and source conditions
Forward Looking Infrared Radiometer (FLIR) cameras offer a unique view of explosive volcanism by providing an image of calibrated temperatures. In this study, 344 eruptive events at Stromboli volcano, Italy, were imaged in 2001–2004 with a FLIR camera operating at up to 30 Hz. The FLIR was effective at revealing both ash plumes and coarse ballistic scoria, and a wide range of eruption...
Authors
Matthew R. Patrick, Andrew J. L. Harris, Maurizio Ripepe, Jonathan Dehn, David A. Rothery, Sonia Calvari
Introduction--Subduction's sharpest arrow Introduction--Subduction's sharpest arrow
No abstract available.
Authors
J.C. Eichelberger
Volcano deformation--Geodetic monitoring techniques Volcano deformation--Geodetic monitoring techniques
This book describes the techniques used by volcanologists to successfully predict several recent volcanic eruptions by combining information from various scientific disciplines, including geodetic techniques. Many recent developments in the use of state-of-the-art and emerging techniques, including Global Positioning System and Synthetic Aperture Radar Interferometry, mean that most...
Authors
Daniel Dzurisin, Zhong Lu