Using high‐resolution distributed temperature sensing to quantify spatial and temporal variability in vertical hyporheic flux
- 23 February 2012
- journal article
- Published by American Geophysical Union (AGU) in Water Resources Research
- Vol. 48 (2)
- https://doi.org/10.1029/2011wr011227
Abstract
No abstract availableKeywords
This publication has 54 references indexed in Scilit:
- A comparison of fibre‐optic distributed temperature sensing to traditional methods of evaluating groundwater inflow to streamsHydrological Processes, 2011
- Hyporheic Exchange in Mountain Rivers II: Effects of Channel Morphology on Mechanics, Scales, and Rates of ExchangeGeography Compass, 2009
- Transient or steady‐state? Using vertical temperature profiles to quantify groundwater–surface water exchangeHydrological Processes, 2009
- Residence time of bedform-driven hyporheic exchangeAdvances in Water Resources, 2008
- Heat as a tracer to determine streambed water exchangesWater Resources Research, 2008
- Analyzing Bank Filtration by Deconvoluting Time Series of Electric ConductivityGroundwater, 2007
- Heat as a Ground Water TracerGroundwater, 2005
- Impact of heterogeneity, bed forms, and stream curvature on subchannel hyporheic exchangeWater Resources Research, 2004
- Delineating and Quantifying Ground Water Discharge Zones Using Streambed TemperaturesGroundwater, 2004
- Flow reversal over a natural pool–riffle sequence: a computational studyEarth Surface Processes and Landforms, 2003