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).
Transit times and rapid chemical equilibrium explain chemostasis in glacial meltwater streams in the McMurdo Dry Valleys, Antarctica. Geophysical Research Letters 45, 13322 - 13331 (2018).
Soil Moisture Controls the Thermal Habitat of Active Layer Soils in the McMurdo Dry Valleys, Antarctica. Journal of Geophysical Research: Biogeosciences 123, (2018).
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).
Patterns of hydrologic connectivity in the McMurdo dry valleys, Antarctica: a synthesis of 20 years of hydrologic data. Hydrological Processes 30, 2958-2975 (2016).
Hydrologic connectivity and implications for ecosystem processes - Lessons from naked watersheds. Geomorphology 277, 63 - 71 (2017).
Characterizing hyporheic exchange processes using high-frequency electrical conductivity-discharge relationships on subhourly to interannual timescales. Water Resources Research 53, 4124 - 4141 (2017).