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Updated repeat orbit interferometry package released
RO1_PAC V2.3, a Repeat Orbit Interferometry package that allows topographic and surface change researchers to apply Interferometric Synthetic Aperture Radar (InSAR) methods, is now freely availableExpand
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The 2011 Magnitude 9.0 Tohoku-Oki Earthquake: Mosaicking the Megathrust from Seconds to Centuries
Detailed geophysical measurements reveal features of the 2011 Tohoku-Oki megathrust earthquake. Geophysical observations from the 2011 moment magnitude (Mw) 9.0 Tohoku-Oki, Japan earthquake allowExpand
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An InSAR‐based survey of volcanic deformation in the central Andes
We extend an earlier interferometric synthetic aperture radar (InSAR) survey covering about 900 remote volcanos of the central Andes (14°–27°S) between the years 1992 and 2002. Our survey revealsExpand
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Frictional Afterslip Following the 2005 Nias-Simeulue Earthquake, Sumatra
Continuously recording Global Positioning System stations near the 28 March 2005 rupture of the Sunda megathrust [moment magnitude (Mw) 8.7] show that the earthquake triggered aseismic frictionalExpand
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A satellite geodetic survey of large-scale deformation of volcanic centres in the central Andes
Surface deformation in volcanic areas usually indicates movement of magma or hydrothermal fluids at depth. Stratovolcanoes tend to exhibit a complex relationship between deformation and eruptiveExpand
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Localization of gravity and topography: constraints on the tectonics and mantle dynamics of Venus
SUMMARY We develop a method for spatio-spectral localization of harmonic data on a sphere and use it to interpret recent high-resolution global estimates of the gravity and topography of Venus in theExpand
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Deformation due to a pressurized horizontal circular crack in an elastic half-space, with applications to volcano geodesy
We consider deformation due to sill-like magma intrusions using a model of a horizontal circular crack in a semi-infinite elastic solid. We present exact expressions for vertical and horizontalExpand
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Three-dimensional deformation caused by the Bam, Iran, earthquake and the origin of shallow slip deficit
Our understanding of the earthquake process requires detailed insights into how the tectonic stresses are accumulated and released on seismogenic faults. We derive the full vector displacement fieldExpand
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Correction to “Localized gravity/topography admittance and correlation spectra on Mars: Implications for regional and global evolution”
[1] In the paper ‘‘Localized gravity/topography admittance and correlation spectra on Mars: Implications for regional and global evolution’’ by Patrick J. McGovern, Sean C. Solomon, David E. Smith,Expand
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The complete (3-D) surface displacement field in the epicentral area of the 1999 MW7.1 Hector Mine E
We use Interferometric Synthetic Aperture Radar (InSAR) data to derive continuous maps for three orthogonal components of the co-seismic surface displacement field due to the 1999 M_w7.1 Hector MineExpand
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