Search engine for discovering works of Art, research articles, and books related to Art and Culture
ShareThis
Javascript must be enabled to continue!

Riparian monitoring of wadeable streams on the Fremont River, Capitol Reef National Park, 2009?2021

View through CrossRef
The goal of Northern Colorado Plateau Network (NCPN) riparian monitoring is to deter-mine long-term trends in hydrologic, geomorphic, and vegetative properties of wadeable streams in the context of changes in other ecological drivers, stressors, and processes. This information is intended to provide early warning of resource degradation and determine natural variability of wadeable streams. This report summarizes NCPN monitoring of the Fremont River in Capitol Reef National Park (NP) from water years 2009 to 2021. The focus of this report is to (1) examine patterns in water availability at one monitoring reach from 2010 to 2021, and (2) present geomorphology and vegetation data from four reaches monitored from 2009 to 2021. Vegetation sampling and geomorphology surveys were completed at varying intervals throughout the time period; this report looks at changes within single reaches and establishes a baseline for future comparisons. There are four monitoring reaches established on the Fremont River: (1) F-01, approximately 2.5 kilometers upstream of a knickpoint (sharp change in channel slope) and associated waterfall that emerged following construction of State Highway 24 in 1964, (2) F-07, in a large oxbow that was cut off due to the highway construction, (3) F-04, approximately 1.5 kilometers downstream of the knickpoint, and (4) F-14, approximately 4.8 kilometers downstream of the knickpoint. Geomorphic and vegetation surveys took place at all reaches. Hydrologic monitoring occurred only at F-01. From 2001 to 2021, the entire range of flows recorded at a gaging station on the Fremont River upstream of the park near Bicknell, Utah, decreased, with the steepest decreases occurring in the highest flow percentiles. Continuous hydrologic monitoring at reach F-01 in the park from 2010 to 2021 showed perennial flows in the Fremont River, with lower flows during the irrigation season (April 1?October 31). The irrigation season was also characterized by greater evapotranspiration, which may be exacerbated in the future due to higher air temperatures. Lower observed inputs and greater evapotranspiration suggest the Fremont River is at risk for progressively lower flows over time. While overbank flows occurred infrequently in the monitoring reach, inhibiting cottonwood recruitment, groundwater levels remained shallow enough to support mature cottonwood trees. Protecting spring snowmelt flows of 94 cfs (the average annual maximum 14-day rolling mean at reach F-01), or greater should maintain the current wetland vegetated zone. Maintaining the hydrologic record was challenging due to high-magnitude flood events and turbid flows; the park should consider a gaging station for an accurate discharge record. Geomorphic surveys showed net sediment deposition at reaches F-01 and F-14 in the channels, banks, and floodplains from 2009 to 2021, with more deposition occurring earlier in the study period. A large flood event in 2013 resulted in high flows and deposition of close to one meter at F-01. Only localized erosion occurred, and thalweg surveys showed that stream channels were either stable or increasing in elevation. Reach F-07, the abandoned oxbow, exhibited little geomorphic change over the study period. Riparian vegetation was characteristic of a Fremont cottonwood woodland, with canopy closure up to 30% and a mixed understory of shrubs and herbaceous species. Obligate wetland vegetation cover of 5%?10% was present at reaches F-01, F-04, and F-14. Reach F-07, in the oxbow, has transitioned to an upland system, with little to no canopy cover and no obligate wetland species. While mature cottonwoods were present in reaches F-01, F-04, and F-14, there was limited evidence of seedlings or saplings graduating into larger size classes. Cottonwood seedlings are primarily resprouts from beaver-browsed trees, although one seedling recruitment event was observed in 2014, following high flows in late 2013. Protecting some cottonwoods with chicken wire may help protect the larger size classes and maintain a mixed-age woodland. Exotic plant species cover was less than 10% in reaches F-01, F-04, and F-14. Efforts to control Russian olive (Eleagnus angustifolia) along the Fremont River appear to have been successful in these reaches. In reach F-07, exotic plant cover ranged from 9% to 25%, with notable spikes in Russian thistle (Salsola tragus) and cheatgrass (Bromus tectorum) in 2010 and 2011, respectively.
Title: Riparian monitoring of wadeable streams on the Fremont River, Capitol Reef National Park, 2009?2021
Description:
The goal of Northern Colorado Plateau Network (NCPN) riparian monitoring is to deter-mine long-term trends in hydrologic, geomorphic, and vegetative properties of wadeable streams in the context of changes in other ecological drivers, stressors, and processes.
This information is intended to provide early warning of resource degradation and determine natural variability of wadeable streams.
This report summarizes NCPN monitoring of the Fremont River in Capitol Reef National Park (NP) from water years 2009 to 2021.
The focus of this report is to (1) examine patterns in water availability at one monitoring reach from 2010 to 2021, and (2) present geomorphology and vegetation data from four reaches monitored from 2009 to 2021.
Vegetation sampling and geomorphology surveys were completed at varying intervals throughout the time period; this report looks at changes within single reaches and establishes a baseline for future comparisons.
There are four monitoring reaches established on the Fremont River: (1) F-01, approximately 2.
5 kilometers upstream of a knickpoint (sharp change in channel slope) and associated waterfall that emerged following construction of State Highway 24 in 1964, (2) F-07, in a large oxbow that was cut off due to the highway construction, (3) F-04, approximately 1.
5 kilometers downstream of the knickpoint, and (4) F-14, approximately 4.
8 kilometers downstream of the knickpoint.
Geomorphic and vegetation surveys took place at all reaches.
Hydrologic monitoring occurred only at F-01.
From 2001 to 2021, the entire range of flows recorded at a gaging station on the Fremont River upstream of the park near Bicknell, Utah, decreased, with the steepest decreases occurring in the highest flow percentiles.
Continuous hydrologic monitoring at reach F-01 in the park from 2010 to 2021 showed perennial flows in the Fremont River, with lower flows during the irrigation season (April 1?October 31).
The irrigation season was also characterized by greater evapotranspiration, which may be exacerbated in the future due to higher air temperatures.
Lower observed inputs and greater evapotranspiration suggest the Fremont River is at risk for progressively lower flows over time.
While overbank flows occurred infrequently in the monitoring reach, inhibiting cottonwood recruitment, groundwater levels remained shallow enough to support mature cottonwood trees.
Protecting spring snowmelt flows of 94 cfs (the average annual maximum 14-day rolling mean at reach F-01), or greater should maintain the current wetland vegetated zone.
Maintaining the hydrologic record was challenging due to high-magnitude flood events and turbid flows; the park should consider a gaging station for an accurate discharge record.
Geomorphic surveys showed net sediment deposition at reaches F-01 and F-14 in the channels, banks, and floodplains from 2009 to 2021, with more deposition occurring earlier in the study period.
A large flood event in 2013 resulted in high flows and deposition of close to one meter at F-01.
Only localized erosion occurred, and thalweg surveys showed that stream channels were either stable or increasing in elevation.
Reach F-07, the abandoned oxbow, exhibited little geomorphic change over the study period.
Riparian vegetation was characteristic of a Fremont cottonwood woodland, with canopy closure up to 30% and a mixed understory of shrubs and herbaceous species.
Obligate wetland vegetation cover of 5%?10% was present at reaches F-01, F-04, and F-14.
Reach F-07, in the oxbow, has transitioned to an upland system, with little to no canopy cover and no obligate wetland species.
While mature cottonwoods were present in reaches F-01, F-04, and F-14, there was limited evidence of seedlings or saplings graduating into larger size classes.
Cottonwood seedlings are primarily resprouts from beaver-browsed trees, although one seedling recruitment event was observed in 2014, following high flows in late 2013.
Protecting some cottonwoods with chicken wire may help protect the larger size classes and maintain a mixed-age woodland.
Exotic plant species cover was less than 10% in reaches F-01, F-04, and F-14.
Efforts to control Russian olive (Eleagnus angustifolia) along the Fremont River appear to have been successful in these reaches.
In reach F-07, exotic plant cover ranged from 9% to 25%, with notable spikes in Russian thistle (Salsola tragus) and cheatgrass (Bromus tectorum) in 2010 and 2011, respectively.

Related Results

Riparian monitoring of wadeable streams protocol for park units in the Northern Colorado Plateau Network: Version 1.06
Riparian monitoring of wadeable streams protocol for park units in the Northern Colorado Plateau Network: Version 1.06
Because of the scarcity of water on the Colorado Plateau and their disproportionately high use by flora and fauna, riparian areas were quickly identified as an ecosystem of concern...
Modelling regime shifts of coral reefs to sponge reefs
Modelling regime shifts of coral reefs to sponge reefs
<p>Coral reef ecosystems have been degrading globally for decades due to global climate change and anthropogenic pressure, and corals are expected to continue declining in th...
Can cows and fish co-exist?
Can cows and fish co-exist?
Our paper provides an ecological perspective on the interrelationship between livestock grazing and riparian areas through a review of topical literature. We also describe the Albe...
United States Capitol and Campus
United States Capitol and Campus
The United States Capitol, located in Washington, DC, houses the US Congress. Congress is the legislative branch of the federal government whose job is to pass laws and serve as th...
Wadeable stream habitat monitoring at Chattahoochee River National Recreation Area: 2021 change report
Wadeable stream habitat monitoring at Chattahoochee River National Recreation Area: 2021 change report
The Southeast Coast Network (SECN) stream habitat monitoring protocol collects data to give park resource managers insight into the status of and trends in stream and near-channel ...
Coral Reef Viruses in Kane'ohe Bay, Hawai'i: Abundance, Diversity & Environmental Drivers
Coral Reef Viruses in Kane'ohe Bay, Hawai'i: Abundance, Diversity & Environmental Drivers
<p>Viruses are a ubiquitous component of coral reef ecosystems, with several viral types, from at least seven prokaryotic and 20 eukaryotic virus families currently character...
Coral Reef Viruses in Kane'ohe Bay, Hawai'i: Abundance, Diversity & Environmental Drivers
Coral Reef Viruses in Kane'ohe Bay, Hawai'i: Abundance, Diversity & Environmental Drivers
<p>Viruses are a ubiquitous component of coral reef ecosystems, with several viral types, from at least seven prokaryotic and 20 eukaryotic virus families currently character...

Back to Top