Soil Moisture Controls the Thermal Habitat of Active Layer Soils in the McMurdo Dry Valleys, Antarctica. Journal of Geophysical Research: Biogeosciences 123, (2018).
Transit times and rapid chemical equilibrium explain chemostasis in glacial meltwater streams in the McMurdo Dry Valleys, Antarctica. Geophysical Research Letters 45, 13,322 - 13,331 (2018).
Characterizing hyporheic exchange processes using high-frequency electrical conductivity-discharge relationships on subhourly to interannual timescales. Water Resources Research 53, 4124 - 4141 (2017).
Hydrologic connectivity and implications for ecosystem processes - Lessons from naked watersheds. Geomorphology 277, 63 - 71 (2017).
Hydrologic connectivity in the McMurdo Dry Valleys, Antarctica: Water-mediated mass and energy fluxes in streams and soils. Department of Civil, Environmental, and Architectural Engineering Ph.D., (2017).
Patterns of hydrologic connectivity in the McMurdo dry valleys, Antarctica: a synthesis of 20 years of hydrologic data. Hydrological Processes 30, 2958-2975 (2016).
Potential for real-time understanding of coupled hydrologic and biogeochemical processes in stream ecosystems: Future integration of telemetered data with process models for glacial meltwater streams. Water Resources Research 51, 6725 - 6738 (2015).