Part of a series of articles titled Park Air Profiles.
Article
Park Air Profiles - Canyonlands National Park
Air Quality at Canyonlands National Park
Most visitors expect clean air and clear views in parks. Canyonlands National Park (NP), Utah, is a wilderness of countless canyons and fantastically formed buttes carved by the Colorado River and its tributaries. Upwind emissions from disturbed dry lands, oil and gas development, and regional wildfires, as well as urban and industrial sources all contribute to air pollution in the park. Airborne pollutants can harm the park’s natural and scenic resources such as soils, surface waters, vegetation, and visibility. The National Park Service works to address air pollution effects at Canyonlands NP, and in parks across the U.S., through science, policy and planning, and by doing our part.
Nitrogen and Sulfur
Nitrogen (N) and sulfur (S) compounds deposited from the air may have harmful effects on ecosystem processes. Healthy ecosystems can naturally buffer a certain amount of pollution, but once a threshold is passed the ecosystem may respond negatively. This threshold is the critical load, or the amount of pollution above which harmful changes in sensitive ecosystems occur (Porter 2005). N and S deposition change ecosystems through eutrophication (N deposition) and acidification (N + S deposition). Eutrophication increases soil and water nutrients which causes some species to grow more quickly and changes community composition. Ecosystem sensitivity to nutrient N enrichment at Canyonlands National Park (CANY) relative to other national parks is very high (Sullivan et al. 2016); for a full list of N sensitive ecosystem components, see: NPS ARD 2019. Acidification leaches important cations from soils, lakes, ponds, and streams which decreases habitat quality. Ecosystem sensitivity to acidification at CANY relative to other national parks is moderate (Sullivan et al. 2016); to search for acid-sensitive plant species, see: NPSpecies.
From 2017-2019 total N deposition in CANY ranged from 2.0 to 2.6 kg-N ha-1 yr-1 and total S deposition ranged from 0.5 to 0.8 kg-S ha-1 yr-1 based on the TDep model (NADP, 2018). CANY has been monitoring atmospheric N and S deposition since 1997, see the conditions and trends website for park-specific information.
Arid ecosystems have shown variable responses to excess N. Research conducted near CANY found that experimental N additions resulted in unexpectedly large increases in the growth of invasive exotic Russian thistle, also known as tumbleweed (Schwinning et al. 2005). This finding is similar to results of research conducted in the Mojave Desert, where N deposition has been found to promote the spread of fast-growing exotic annual grasses such as red brome (Brooks 2003, Allen et al. 2009). In contrast, a recent study showed little vegetation response to fertilization, but did see a decline in the stability of the soil crust community (Phillips et al. 2021). Plant community structure in the region is resistant to chronic N additions at and above the estimated critical load, suggesting a relatively low sensitivity of these dryland plants to added N (Phillips et al. 2021).
Given the abundance of base cations in underlying park soils and rocks, surface waters in CANY are generally well-buffered from acidification. However, the park's small pothole aquatic systems may be sensitive to incoming acid inputs. Additionally, small streams with steep-sided canyon walls in CANY have little ability to retain nutrients and water, offering the landscape little opportunity to buffer potentially acidic run-off (Sullivan et al. 2016).
Epiphytic macrolichen community responses
Epiphytic macrolichens grow on tree trunks, branches, and boles. Since these lichens grow above the ground, they obtain all their nutrients directly from precipitation and the air. Many epiphytic lichen species have narrow environmental niches and are extremely sensitive to changes in air pollution. Epiphytic lichen communities are less diverse in arid areas, but are still impacted by air pollution. Geiser et al. (2019) used a U.S. Forest Service national survey to develop critical loads of nitrogen (N) and critical loads of sulfur (S) to prevent more than a 20% decline in four lichen community metrics: total species richness, pollution sensitive species richness, forage lichen abundance, and cyanolichen abundance.
McCoy et al. (2021) used forested area from the National Land Cover Database to estimate the impact of air pollution on epiphytic lichen communities. Forested area makes up 68 km2 (4.9%) of the land area of Canyonlands National Park.
- N deposition was below the 3.1 kg-N ha-1 yr-1 critical load to protect N-sensitive lichen species richness in every part of the forested area.
- S deposition was below the 2.7 kg-S ha-1 yr-1 critical load to protect S-sensitive lichen species richness in every part of the forested area.
For exceedances of other lichen metrics and the predicted decline of lichen communities see Appendices A and B of McCoy et al. (2021).
Additional modeling was done on 459 lichen species to test the combined effects of air pollution and climate gradients (Geiser et al. 2021). A critical load indicative of initial shifts from pollution-sensitive toward pollution-tolerant species occurred at 1.5 kg-N ha-1 yr-1 and 2.7 kg-S ha-1 yr-1 even under changing climate regimes.
Plant species response
Plants vary in their tolerance of eutrophication and acidification, and some plant species respond to nitrogen (N) or sulfur (S) pollution with declines in growth, survival, or abundance on the landscape. Horn et al. (2018) used the U.S. Forest Service national forest survey to develop critical loads of N and critical loads of S to prevent declines in growth or survival of sensitive tree species. Clark et al. (2019) used a database of plant community surveys to develop critical loads of N and critical loads of S to prevent a decline in abundance of sensitive herbaceous plant species. According to NPSpecies, Canyonlands National Park contains:
- 2 N-sensitive tree species and 12 N-sensitive herbaceous species.
- 6 S-sensitive tree species and 12 S-sensitive herbaceous species.
Mycorrhizal fungi community response
Many plants have a symbiotic relationship with mycorrhizal fungi (MF). Through the roots, the plants supply the fungi with carbon from photosynthesis and in exchange the MF enhance nutrient availability within soils, increase drought tolerance, and provide physical resistance to soil erosion (George et al., 1995; Cheng et al., 2021; Burri et al., 2013). Anthropogenic Nitrogen (N) deposition can disrupt this symbiotic relationship resulting in a shift from N sensitive to N tolerant mycorrhizal fungi and plant communities.
With increased N deposition to the soil, MF become less important for nutrient uptake and many plants will cease the exchange of nutrients altogether making them more vulnerable to stressors such as drought (Lilleskov et al., 2019). The CL-N for the shift in mycorrhizal community is 5-6 kg-N ha-1 yr-1 in coniferous forests and 10-20 kg-N ha-1 yr-1 broadleaf forests.
Canyonlands National Park has 217.8 km2 of coniferous forests and 0.4 km2 of broadleaf forests. Using the range in critical loads above, the minimum CL is exceeded in 0% of forested area and the maximum CL is exceeded in 0% of forested area based on 2019-2021 TDep Total N deposition.
Change in N and S deposition from 2000 to 2021
The maps below show how the spatial distribution of estimated Total N and Total S deposition in CANY has changed from 2000-2002 to 2019-2021 (TDep MMF version 2022.02). Slide the arrows in the middle of the image up and down to compare N and S deposition between the two years (Yearly Data).
- Minimum N deposition decreased from 2.1 to 1.4 kg-N ha-1 yr-1 and maximum N deposition decreased from 3.4 to 2.7 kg-N ha-1 yr-1.
- Minimum S deposition decreased from 0.7 to 0.3 kg-S ha-1 yr-1 and maximum S deposition decreased from 0.9 to 0.5 kg-S ha-1 yr-1.
Persistent Pollutants
Pollutants like mercury and pesticides are concerning because they are persistent and toxic in the environment. These contaminants can travel in the air thousands of miles away from the source of pollution, even depositing in protected places like national parks. In addition, while some of these harmful pollutants may be banned from use, historically contaminated sites continue to endure negative environmental consequences.
When deposited, airborne mercury and other toxic air contaminants are known to harm wildlife like birds and fish, and cause human health concerns. Many of these substances enter the food chain and accumulate in the tissue of organisms causing reduced reproductive success, impaired growth and development, and decreased survival.
- Microplastics were found in park precipitation samples. These microplastics, thought to be distributed by atmospheric transport, consisted mostly of clothing fibers like cotton, polyester, and nylon. Canyonlands NP is estimated to have an annual deposition rate of 1.2-1.5 metric tons of plastic per year (Brahney et al. 2020).
- Contaminants of emerging concern (CECs), some of which are known toxins and thought to be atmospherically transported, have been found in park surface water and sediment samples. CECs include pharmaceuticals and personal care products (PPCPs), wastewater indicators (WWIs), and pesticides. Some CECs consistently found in/near Canyonlands include the pesticide triclopyr and various pharmaceuticals (Northern Colorado Plateau Inventory and Monitoring Program 2018; Weissinger et al. 2018; Weissinger et al. 2016).
- Fish consumption advisories may be in effect for mercury and other contaminants (NPS 2022).
The NPS Air Resources Division reports on park conditions and trends for mercury. Visit the webpage to learn more.
Visibility
Visitors come to Canyonlands NP, a high desert on the Colorado Plateau in Utah, to enjoy scenic views of spectacular canyons, mesas, needle-like spires, and deep river gorges. Park vistas are sometimes obscured by haze, reducing how well and how far people can see. Visibility reducing haze is caused by tiny particles in the air, and these particles can also affect human health. Many of the same pollutants that ultimately fall out as nitrogen and sulfur deposition contribute to this haze. Organic compounds, soot, dust, and wood smoke reduce visibility as well.
Arid environments, including most of the Colorado Plateau region surrounding Canyonlands NP, often experience airborne dust due to long-term aridity, sparse plant cover, and sensitive soil surfaces (Neff et al. 2013). Soil disturbances and severe wind episodes can increase dust concentrations but vary greatly in both space and time (Flagg et al. 2014). The U.S. Geological Survey (USGS) is currently monitoring patterns of dust emissions within and outside the park to more thoroughly understand background emission levels, seasonal dynamics, and other factors that may influence timing and levels of dust in the air. USGS scientists are using field, laboratory, and statistical modeling methods to carry out this work. A related research project is measuring the effect of vehicle-use and surface conditions on unpaved roads on dust emissions in and around Canyonlands NP.
Significant improvements in park visibility have been documented since the early 1990’s. Overall, visibility in the park still needs some improvement to reach the Clean Air Act goal of no human caused impairment.
Visibility effects:
- Reduced visibility, at times, due to human-caused haze from dust and other fine particles of air pollution;
- Reduction of the average natural visual range from about 175 miles (without pollution) to about 130 miles because of airborne pollutants that impact the park’s viewshed;
- Reduction of the visual range to below 90 miles on high pollution days.
Visit the NPS air quality conditions and trends website for park-specific visibility information. Canyonlands NP has been monitoring visibility since 1989. View a live dust monitoring webcam and explore air monitoring »
Ground-Level Ozone
At ground level, ozone is harmful to human health and the environment. Ground-level ozone does not come directly from smokestacks or vehicles, but instead is formed when other pollutants, mainly nitrogen oxides and volatile organic compounds, react in the presence of sunlight.
Over the course of a growing season, ozone can damage plant tissues making it harder for plants to produce and store food. It also weakens plants making them less resistant to disease and insect infestations. Some plants are more sensitive to ozone than others. A risk assessment that considered ozone exposure, soil moisture, and sensitive plant species concluded that plants in Canyonlands NP were at low risk of ozone injury (Kohut 2007; Kohut 2004). However, estimated ozone concentrations and cumulative doses at the park are high enough to damage the leaves of sensitive vegetation under certain conditions. Dry conditions in the park generally limit plant respiration and ozone uptake. But, in moist areas along streams and seeps, plants may be more vulnerable to ozone leaf damage (Kohut et al. 2012). Ozone sensitive plant species at the park include Salix gooddingii (Goodding’s willow) and Fraxinus anomala (Singleleaf ash). Search for more ozone-sensitive plant species found at Canyonlands NP.
Visit the NPS air quality conditions and trends website for park-specific ozone information. Canyonlands NP has been monitoring ozone since 1992. View live ozone and meteorology data and explore air monitoring »
Explore Other Park Air Profiles
There are 47 other Park Air Profiles covering parks across the United States and its territories.
References
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Brooks, M.L. 2003. Effects of increased soil nitrogen on the dominance of alien annual plants in the Mojave Desert. Journal of Applied Ecology. 40:344–353.
Burri, K., C. Gromke, and F. Graf. "Mycorrhizal fungi protect the soil from wind erosion: a wind tunnel study." Land Degradation & Development 24.4 (2013): 385-392.
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Last updated: August 6, 2024