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Applying UV cameras for SO2 detection to distant or optically thick volcanic plumes Applying UV cameras for SO2 detection to distant or optically thick volcanic plumes

Ultraviolet (UV) camera systems represent an exciting new technology for measuring two dimensional sulfur dioxide (SO2) distributions in volcanic plumes. The high frame rate of the cameras allows the retrieval of SO2 emission rates at time scales of 1 Hz or higher, thus allowing the investigation of high-frequency signals and making integrated and comparative studies with other high-data...
Authors
Christoph Kern, Cynthia Werner, Tamar Elias, A. Jeff Sutton, Peter Lübcke

Geochronologic and geochemical data from Mesozoic rocks in the Black Mountain area northeast of Victorville, San Bernardino County, California Geochronologic and geochemical data from Mesozoic rocks in the Black Mountain area northeast of Victorville, San Bernardino County, California

We present geochronologic and geochemical data for Mesozoic rocks in the Black Mountain area northeast of Victorville, California, to supplement previous geologic mapping. These data, together with previously published results, limit the depositional age of the sedimentary Fairview Valley Formation to Early Jurassic, refine the ages and chemical compositions of selected units in the...
Authors
Paul Stone, Andrew P. Barth, Joseph L. Wooden, Nicole K. Fohey-Breting, Jorge A. Vazquez, Susan S. Priest

Exploring Hawaiian volcanism Exploring Hawaiian volcanism

In 1912 the Hawaiian Volcano Observatory (HVO) was established by Massachusetts Institute of Technology professor Thomas A. Jaggar Jr. on the island of Hawaii. Driven by the devastation he observed while investigating the volcanic disasters of 1902 at Montagne Pelée in the Caribbean, Jaggar conducted a worldwide search and decided that Hawai‘i provided an excellent natural laboratory for
Authors
Michael P. Poland, Paul G. Okubo, Ken Hon

The role of viscous magma mush spreading in volcanic flank motion at Kīlauea Volcano, Hawai‘i The role of viscous magma mush spreading in volcanic flank motion at Kīlauea Volcano, Hawai‘i

Multiple mechanisms have been suggested to explain seaward motion of the south flank of Kīlauea Volcano, Hawai‘i. The consistency of flank motion during both waxing and waning magmatic activity at Kīlauea suggests that a continuously acting force, like gravity body force, plays a substantial role. Using finite element models, we test whether gravity is the principal driver of long-term...
Authors
C. Plattner, F. Amelung, S. Baker, R. Govers, Michael P. Poland

Reorganization of vegetation, hydrology and soil carbon after permafrost degradation across heterogeneous boreal landscapes Reorganization of vegetation, hydrology and soil carbon after permafrost degradation across heterogeneous boreal landscapes

The diversity of ecosystems across boreal landscapes, successional changes after disturbance and complicated permafrost histories, present enormous challenges for assessing how vegetation, water and soil carbon may respond to climate change in boreal regions. To address this complexity, we used a chronosequence approach to assess changes in vegetation composition, water storage and soil...
Authors
M.T. Jorgenson, Jennifer W. Harden, M. Kanevskiy, J.A. O'Donnell, Kimberly Wickland, S. Ewing, Kristen L. Manies, Q. Zhuang, Y. Shur, Robert G. Striegl, Joshua C. Koch

Evolution of dike opening during the March 2011 Kamoamoa fissure eruption, Kīlauea Volcano, Hawai`i Evolution of dike opening during the March 2011 Kamoamoa fissure eruption, Kīlauea Volcano, Hawai`i

The 5–9 March 2011 Kamoamoa fissure eruption along the east rift zone of Kīlauea Volcano, Hawai`i, followed months of pronounced inflation at Kīlauea summit. We examine dike opening during and after the eruption using a comprehensive interferometric synthetic aperture radar (InSAR) data set in combination with continuous GPS data. We solve for distributed dike displacements using a whole...
Authors
Paul Lundgren, Michael P. Poland, Asta Miklius, Tim R. Orr, Sang-Ho Yun, Eric Fielding, Zhen Liu, Akiko Tanaka, Walter Szeliga, Scott Hensley, Susan Owen

Bayesian inversion of data from effusive volcanic eruptions using physics-based models: Application to Mount St. Helens 2004--2008 Bayesian inversion of data from effusive volcanic eruptions using physics-based models: Application to Mount St. Helens 2004--2008

Physics-based models of volcanic eruptions can directly link magmatic processes with diverse, time-varying geophysical observations, and when used in an inverse procedure make it possible to bring all available information to bear on estimating properties of the volcanic system. We develop a technique for inverting geodetic, extrusive flux, and other types of data using a physics-based...
Authors
Kyle Anderson, Paul Segall

Modeling crustal deformation near active faults and volcanic centers: a catalog of deformation models and modeling approaches Modeling crustal deformation near active faults and volcanic centers: a catalog of deformation models and modeling approaches

This manual provides the physical and mathematical concepts for selected models used to interpret deformation measurements near active faults and volcanic centers. The emphasis is on analytical models of deformation that can be compared with data from the Global Positioning System (GPS) receivers, Interferometric synthetic aperture radar (InSAR), leveling surveys, tiltmeters and...
Authors
Maurizio Battaglia, Peter F. Cervelli, Jessica R. Murray

Overview of Chaitén Volcano, Chile, and its 2008-2009 eruption Overview of Chaitén Volcano, Chile, and its 2008-2009 eruption

Chaitén Volcano erupted unexpectedly in May 2008 in one of the largest eruptions globally since the 1990s. It was the largest rhyolite eruption since the great eruption of Katmai Volcano in 1912, and the first rhyolite eruption to have at least some of its aspects monitored. The eruption consisted of an approximately 2-week-long explosive phase that generated as much as 1 km3 bulk volume...
Authors
Jon J. Major, Luis E. Lara

Merapi 2010 eruption—Chronology and extrusion rates monitored with satellite radar and used in eruption forecasting Merapi 2010 eruption—Chronology and extrusion rates monitored with satellite radar and used in eruption forecasting

Despite dense cloud cover, satellite-borne commercial Synthetic Aperture Radar (SAR) enabled frequent monitoring of Merapi volcano's 2010 eruption. Near-real-time interpretation of images derived from the amplitude of the SAR signals and timely delivery of these interpretations to those responsible for warnings, allowed satellite remote sensing for the first time to play an equal role...
Authors
John S. Pallister, David J. Schneider, Julia P. Griswold, Ronald H. Keeler, William C. Burton, Christopher Noyles, Christopher G. Newhall, Antonius Ratdomopurbo

Integrating satellite observations and modern climate measurements with the recent sedimentary record: An example from Southeast Alaska Integrating satellite observations and modern climate measurements with the recent sedimentary record: An example from Southeast Alaska

Assessments of climate change over time scales that exceed the last 100 years require robust integration of high-quality instrument records with high-resolution paleoclimate proxy data. In this study, we show that the recent biogenic sediments accumulating in two temperate ice-free fjords in Southeast Alaska preserve evidence of North Pacific Ocean climate variability as recorded by both
Authors
Jason A. Addison, Bruce P. Finney, John M. Jaeger, Joseph S. Stoner, Richard D. Norris, Alexandra Hangsterfer

The 2010 eruption of Merapi volcano The 2010 eruption of Merapi volcano

We briefly present the normal eruption of Merapi volcano. We summarize the 2010 eruption. We list the contribution of the Special Issue of JVGR on the 2010 eruption of Merapi volcano.
Authors
Philippe Jousset, John S. Pallister, Surono
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