Outreach

In order to foment discussion and disseminate our findings we have presented our work at a variety of community, agency and academic forums.

Tribal Wetlands Working Group (TWIG) Tour of Meacham Creek Restoration work.

Presentations through the Years………

How to think about hyporheic exchange in gravel bedded rivers.

Is floodplain sediment important for stream channel temperatures?

A comparison of channel shade and hyporheic exchange on seasonal patterns of stream temperature.

When and how dynamic hyporheic temperature mosaics influence channel temperature regimes. 

When and how dynamic hyporheic temperature mosaics influence channel temperature regimes. 

Selecting Annual Temperature Signals for Inverse Modeling of Aquifer Hydraulic Properties.

A Novel Approach to Simulating Hyporheic Influences on Stream Channel Temperature. 

Meacham Creek Hyporheic Restoration and Monitoring.

Limits of Transient Storage Assumptions for Heat: Using Residence Time Distribution to Estimate Mean Temperature of Hyporheic Discharge in Montane Alluvial Streams.

Use of Annual Hyporheic Temperature Signals to Evaluate the Effects of Channel Realignment.

A Novel Approach to Simulating Hyporheic Influences on Stream Channel Temperature. 

Meacham Creek Hyporheic Restoration Monitoring Project.

Predicting Water Movement throughout Coarse-Grained Alluvial Aquifers Via Analysis of Annual Temperature Signals.

Characterizing Hyporheic Effects on Diel and Annual Stream Temperature Cycles Across Variable Channel Morphology and Aquifer Characteristics.

The Importance of Thermal Dispersivity in Predicting Water Movement through Coarse-grained Alluvial Aquifers by Analysis of Seasonal Temperature Signals.

Stream Temperature “Hysteresis Plots” as a Tool for Inferring Hyporheic Exchange in a Restored River. 

Reconfigured Groundwater Hydrology and Energy Dynamics in a Restored Western River.

Flowpaths, Lagrangian Hydrology, and Hyporheic Dynamics; or, Why Your Hyporheic Monitoring Data Might Not Make Sense. 

Preliminary Simulation of Hyporheic Hydrology Suggests Systematic Changes in Hyporheic Flow Path Residence Time in Response to Reach-Scale Channel Restoration. 

Modeling Interactions between Surface and Subsurface Temperature Dynamics in Floodplains.

Geomorphology and hyporheic exchange drive whole-river water temperature dynamics in a mainstem gravel-bedded river.

Surface hydrology of low-relief landscapes: an assessment of hydrologic connectivity and flow impedance using LIDAR-derived digital elevation models. 

Synergies of excess sediment and nitrogen: degraded hyporheic dynamics and compromised river ecosystem resilience. 

Synergies of excess sediment and nitrogen: an overview of on-going research from the Umatilla River, Oregon, USA.

An integrated simulation model of stream channel and hyporheic geomorphology, hydrology, temperature, and biogeochemical processing.

Development of a general modeling framework for investigating complex interactions among biological and physical ecosystem dynamics.

Hyporheic hydrology of the Umatilla River: interactions among physical and biological drivers.

Geomorphic and hyporheic controls on water temperature in fluvial landscapes. 

The effect of geomorphic complexity on water temperature in a pacific northwest alluvial river.

Urbanization alters the influence of riparian forest cover on stream temperature dynamics.

Spatiotemporal variation in channel-aquifer hydrologic connectivity within the hyporheic zone of an alluvial river. 

Seasonal variation in water sources within the hyporheic and perirheic zones of an alluvial floodplain.