M
Mark Simons
Researcher at California Institute of Technology
Publications - 186
Citations - 13882
Mark Simons is an academic researcher from California Institute of Technology. The author has contributed to research in topics: Interferometric synthetic aperture radar & Slip (materials science). The author has an hindex of 63, co-authored 176 publications receiving 11943 citations. Previous affiliations of Mark Simons include Massachusetts Institute of Technology.
Papers
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Journal ArticleDOI
Importance of ocean tidal load corrections for differential InSAR
Christopher Dicaprio,Mark Simons +1 more
TL;DR: In this article, the effects of ground displacements due to ocean tidal loads (OTL) were investigated and the importance of OTL with predicted displacements from selected regions of tectonic interest.
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Modeling the elastic transmission of tidal stresses to great distances inland in channelized ice streams
TL;DR: In this paper, a hydrologic model based on time-dependent variability in till strength is proposed to explain transmission of tidal stresses inland of the grounding line, which can reproduce observations from Rutford Ice Stream.
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Interseismic loading of subduction megathrust drives long term uplift in northern Chile
Romain Jolivet,Romain Jolivet,Mark Simons,Zacharie Duputel,J.-A. Olive,Harsha S. Bhat,Quentin Bletery +6 more
TL;DR: In this paper, a potential correlation between long-term, inelastic and short-term interseismic vertical rates in northern Chile is reported, suggesting topography of the forearc builds up during the interseistic period.
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Revisiting the 1992 Landers earthquake: a Bayesian exploration of co-seismic slip and off-fault damage
TL;DR: In this article, a coseismic model obtained from the joint inversion of multiple observations in a relatively unregularized and fully Bayesian framework was proposed to limit the impact of modelling uncertainties.
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Tidal modulation of ice shelf buttressing stresses
TL;DR: In this article, the authors show that nonlinear variations in ice shelf buttressing driven by tides can produce such fortnightly variations in iceberg flow, which is caused by asymmetries in the contact stress from migration of the grounding line and bathymetric pinning points beneath the ice shelf.