Hydrological Linkages Between Landscapes and Stream Networks
Project
Title: Collaborative
Research: Hydrological linkages between landscapes and streams:
Transferring reach and plot scale understanding to the network and
catchment scales
Project
Duration: 1-Apr-2004 - 31-Mar-2008
| Principal
Investigators: Michael Gooseff (Penn State University)
Collaborators: Jan Seibert (Swedish University of Agricultural Sciences) Ken Bencala (NRP, USGS) Steve Wondzell (USFS) Markus Weiler (UBC) Overview: Streams, riparian zones, and hillslopes have been intensively studied at small spatial scales (stream reaches <1 km, plots of a few m2). At the other end of the spectrum, entire catchments have been studied without explicit understanding of how different landscape units interact. In this project, we will address the connections between stream networks, riparian zones and hillslope landscape units. We will address the following questions:
These questions currently limit our ability to transfer our understanding of hydrological processes studied at the plot or reach scale to larger catchments. These questions beg integrated, multi-scale approaches that combine landscape level topographic analysis, process-based field investigations, and catchment-scale integration to identify the factors controlling the hydrologic connectivity between source areas generating runoff and the flow paths that link source areas to streams. Research Site:
We will be conducting our research in the Tenderfoot Creek Experimental Forest in western Montana. |
The
resulting digital elevation map is ~1m resolution! We are currently
using this to perform enhanced landscape analyses.
Field Activities 2004
| On 19-Jun-2004, we
made a preliminary field reconnaissance trip to TCEF. We travelled the
main stem road to the lower Tenderfoot Cr. flume and walked the entire
length of Stringer Cr. [Making water quality, stage, and GPS measurements at Lower Tenderfoot Cr. Flume] |
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![]() Lower Stringer Cr. has a very different stream morphology, such as this step-pool sequence, and narrower riparian zones than... |
![]() ...Upper Stringer Cr., which has a shallower slope, less developed bedform, and flows through wider meadows. |
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The
Lower Stringer Cr., stream gauge has an H-flume, records stage in a
stilling well (inside the gauge house), and records stage from the
sonic sensor that is attached to the tower. In Sept., 2004 we installed a conductivity/temperature probe at this location, as well as at Upper Stringer Cr. stream gauge. |
![]() There are 2 NRCS Snotel sites located in the watershed. This is the installation at Lower Stringer Cr. |
![]() This is the snow pillow, located just to the left of the small data collection house in the picture to the left. |
TCEF Instrumentation and Characteristics
Site
Characteristics:
Existing Data and Equipment Infrastructure
|
SNOTEL Sites within the Forest: |
| Rob Payn, Ph.D student at CSM (current) | Aurora
Bouchier, M.S. student at CSM (current) |
| Kelsey Jencso,
M.S. student at MSU (current) |
Martin
Briggs, M.S. student at CSM (current) |
| Kristen Schmidt, CSM (2005) | |
| Becca McNamara,
MSU (current) |
|
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This project is
funded through the National Science Foundation's Geosciences
Directorate
(EAR-0337781-Gooseff, EAR-0337650 - McGlynn). |