Kristel Chanard has improved our understanding of the role of hydrology in Earth’s space- and time-dependent deformation, gravity field, and rheology. In that endeavor, Kristel’s research has been very much influenced by and followed up on some of John Wahr’s own research. Kristel is exploring how Earth deforms through the development and intelligent use of space geodetic data. The analyses and discussions in her papers are full of interesting points, careful consideration of caveats and related work, and convincing argumentation. She always matches a rigorous observational component in her papers with intriguing and innovative analysis and interpretation. For example, Kristel integrated GPS time series with time-dependent GRACE satellite gravity data from across the India-Tibet collision zone to demonstrate that seasonal hydrological loading variations produce notable annual deformation cycles in both vertical and horizontal components. Importantly, Kristel was able to show that models of the layered elastic Earth structure can be improved by optimizing the fit to phase and amplitude of both vertical and horizontal deformation data. Later, Kristel expanded this approach to the whole Earth, considering nearly 700 GPS stations and complete GRACE gravity data sets. This analysis reconciles the complete 4D surface deformation field and gravity time series through a global elastic spherical and layered Earth model incorporating seasonal elastic deformation and geocenter motion. Finally, she presented a completely new way to examine deep-Earth rheology using geodetic data sets, by developing an approach to estimate short-term asthenospheric viscosity revealed by deformation–gravity phase relations in the seasonal load deformation of Earth. This first analysis of its kind could only provide a lower bound on a global average of short-term asthenospheric viscosity, but opened a whole new window into the workings of the deep Earth. In recent years, Kristel has continued to make valuable contributions at an accelerating pace, including additional studies of seasonal load deformation and seismicity modulations, papers on statistical analyses of seismicity modulation by periodic stresses ranging from tidal to seasonal frequencies, and investigations of Earth orientation parameters and Earth center representations. Kristel has also made impactful contributions to the International Terrestrial Reference Frame, to the rapidly growing field of hydrogeodesy, and to improved understanding of fault zone properties and slip behaviors. Kristel will surely continue to make more insightful contributions to our knowledge of the shape and deformation of Earth.
—Roland Bürgmann, University of California, Berkeley
A tectonic Plate Motion Model (PMM) is essential for geodetic applications, while contributing to the understanding of geodynamic processes affecti...