Current Research
| Photo |
Description |
Link |
 |
Biocomplexity
FLBS colleagues recently received a NSF grant (2001-2004) titled "BIOCOMPLEXITY
-DYNAMIC CONTROLS ON EMERGENT PROPERTIES OF RIVER FLOOD PLAINS" The
fundamental concept of this biocomplexity proposal is that alluvial flood
plains are regional centers of ecological organization, owing to dynamic,
non-linear processes linking water and materials (including biota) flux
and retention (surface and subsurface) to interactive landscape-forming
processes. Specifically, the key processes are cut and fill alluviation,
channel avulsion and production and entrainment of LW (large wood). Groundwater
routing through the flood plain and upwelling back to the surface mainly
involves penetration of river water into zones of high hydraulic conductivity
(paleochannels) created by the legacy of channel scour and fill. The strong
interaction between short-duration, high stream-power floods, channel movement,
increased roughness due to live and dead wood and upwelling of groundwater
creates a complex, dynamic array of resource patches and interfaces, which
we refer to as the shifting habitat mosaic. This mosaic allows many species
to co-exist in the flood plain landscape (biodiversity hotspots). We expect
that biophysical linkages to the shifting habitat mosaic and its drivers
determine flux and storage of heat, oxygen, carbon, nitrogen and phosphorus.
Important modifiers of system dynamics include drought, wildfire, flow and
geomorphic regulation (dams and revetments) and invasions of nonnative species.
|
Full Description |
 |
Effects of climate change on hydrologic systems and associated biota
The purpose of this research is to examine the effects of hydrologic
and thermal change in alpine and subalpine streams and associated
wetlands in McDonald Creek watershed, Glacier National Park. During
the past seven years we have contributed significantly to the
ecological understanding of the stream continuum along the elevation
gradient of this drainage (e.g., Hauer et al. 1997, Fagre et al.
1997, Hauer et al. 1998, Tabbachi et al. 1998, Lowe and Hauer 1999,
Hauer et al 2000). The foundation of this understanding includes
detailed hydrologic and thermal monitoring, repeated measures of
nutrient concentrations and carbon dynamics, and the distribution
and abundance of stream fauna. |
Full Description |
 |
Hydrogeomorphology (HGM) of Wetland Structure and Function
During the past several decades, the scientific community, publics and
government agencies have become aware of the important role wetlands play
in maintaining environmental quality and biotic diversity. This has led
to a societal emphasis on wetland stewardship and management reflected by
increased funding for wetland research and the passage of federal, state
and local laws and ordinances designed to regulate [and minimize]
environmental impacts to wetlands. |
Full Description |
 |
Regulated River EcologyFew changes in the longitudinal dimension of a river have greater
effect than those imposed by dams. Most major rivers of North America have been dramatically altered over the past
century by the construction of dams. The dam-building legacy has left most of the major river systems throughout the
United States, and to a lesser extent Canada, with few free-flowing river systems greater than 4-5th order; a
condition, incidentally, replete throughout western Europe. High-head, hydropower dams have had profound affects
on thermal regimes of rivers throughout North America, particularly in the Pacific Northwest where hypolimnion
release is prevalent among dams draining deep reservoirs. Thermal effects on river tailwaters among mid-reach dams
may extend tens of kilometers downstream influencing productivity and community composition. Indeed the effects of
dams on hydrologic regimes, thermal regimes, nutrient dynamics, sediment transport, and movement of organisms are
profound. This topic has been central to the research efforts at FLBS for over 25 years and will continue to be an
integral part of my research program. These research efforts have taken us throughout the Rocky Mountain west,
central Asia and Europe. |
Full Description |