Coincident aboveground and belowground autonomous monitoring to quantify covariability in permafrost, soil, and vegetation properties in Arctic tundra." Journal of Geophysical Research: Biogeosciences 122, no. 6 (2017): 1321-1342."
Coupled land surface-subsurface hydrogeophysical inverse modeling to estimate soil organic content and explore associated hydrological and thermal dynamics in an Arctic tundra." The Cryosphere Discussions (2017): 1-42."
Estimation of subsurface porosities and thermal conductivities of polygonal tundra by coupled inversion of electrical resistivity, temperature, and moisture content data." The Cryosphere 14, no. 1 (2020): 77-91."
Spatial and temporal variations of thaw layer thickness and its controlling factors identified using time-lapse electrical resistivity tomography and hydro-thermal modeling." Journal of Hydrology 561 (2018): 751-763."