| dc.description.abstract |
Metabolism is a foundational property of ecosystems, and the productivity of rivers
determines their capacity to retain and transform nutrients as well as support biodiversity.
Stream metabolism has been increasingly used to assess waterway health due to its
relevance across sizes and types of streams, sensitivity to stressors, and ability
to be measured continuously. Land use change can affect metabolism through numerous
mechanisms, including hydrology, light regimes, and nutrients, which may respond to
changes in land use at different scales. This study used existing high frequency metabolism
records and geospatial data to examine relationships among measures of catchment and
riparian condition and stream Gross Primary Production (GPP). The primary goals were
to identify the mechanisms by which urbanization and land use change affect metabolism,
the scales at which these drivers exert the most influence, and any variance present
across regions. Quantifiable proxies for each mechanism were used to characterize
and assess its effect on GPP response along an urban land use gradient and spatial
scale.
This study focused on small headwater streams located in mesic environments. The study
area for this project included a collection of stream gage sites in the eastern United
States, each of which is located east of 96 degrees west longitude and has a total
catchment area of less than 26 square kilometers or less. Four primary regions of
focus were selected based on their display of a complete urban gradient (low total
percent urban area to high total percent urban area within the catchment) among stream
gage sites: Atlanta metropolitan area, Kansas City metropolitan area, Mid-Atlantic
region, and Washington D.C. metropolitan area.
Overall, we found that whole watershed scale urban cover was weakly correlated with
stream characteristics that affect metabolism. Total percent tree canopy cover appears
to exert control over metabolism at the local reach scale, while total percent urban
land cover, total percent imperviousness, and total road density do this at the whole
watershed scale. In all cases, GPP was negligible above a threshold land cover, and
the higher variance in GPP at low to moderate urbanization levels is controlled by
local canopy. This suggests that metabolic regimes arise from processes at multiple
scales. Differences in GPP among the four focal regions are likely due to differences
in climate, impervious surface, and riparian canopy among urban areas.
These findings suggest that effective interventions may require catchment scale efforts
to preserve and restore hydrologic regimes as well as local interventions to improve
riparian condition. This has implications for resource protection, mitigation, and
future planning. Understanding the relative importance of these processes and the
scales at which they affect streams is critical for environmental management decisions,
including the conservation and rehabilitation of streams, as well as designing appropriate
interventions. Ultimately, this project demonstrates how richer and larger datasets
can expand our understanding and inform decision making at new scales. Future temporal
scale analyses that assess the seasonality or disturbance recovery trajectories of
these data may further benefit our understanding of these processes and relationships.
Additionally, we suggest conducting comparative analyses of these data in terms of
seasonal patterns and how temporal patterns differ between GPP and ER.
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