In drylands, short-term extreme droughts can have profound ecosystem effects, depending on the timing (seasonality) of drought and the sensitivities of the dominant plants and plant functional types. Past work suggests that cool season drought may disproportionately impact regionally important grass and shrub species. In this study, we are examining the impacts of extreme seasonal drought on grassland communities of the Colorado Plateau. This experiment was established in 2015 at one large site near Canyonlands National Park in southeastern Utah. We are focusing on the impacts of extreme (a 66% reduction in precipitation) warm and cool season drought on grass and mixed grass-shrub communities using large, moveable passive rainfall reduction shelters. This ongoing experiment is part of a larger network imposing extreme drought in grasslands globally (http://edge.biology.colostate.edu/).
Background & Importance
Drylands cover 41% of the terrestrial land surface and are one of the most vulnerable regions to changes precipitation and temperature. These arid and semiarid ecosystems are extremely resource limited, most notably for water, and thus any changes in water availability can lead to large ecological shifts. Like many drylands, the southwestern U.S. is experiencing warming and changes in precipitation. The early (2001-2010) was the warmest decade in in the instrumental record and models predict continued warming for this region. While periods of drought are a climatic feature of the southwest, recent “hot droughts” have had profound impacts on many southwest ecosystems. Grassland on the Colorado Plateau provide a myriad of important ecosystem services, including forage for livestock, habitat for wildlife, and conservation of soil resources. Thus, gaining new insights into drought vulnerabilities of Colorado Plateau grasslands is needed to mitigate deleterious impacts of future droughts.
General Methods
We are imposing extreme seasonal drought by excluding 66% of the natural precipitation using shelters that cover both grasses and shrubs. We have three precipitation treatments: 1) drought during the summer/fall growing season (May – October), 2) drought during the winter/spring cool season (November – April) and 3) ambient. We have applied each of these treatments to two different plant communities: 1) perennial grass community without shrubs and 2) mixed shrub-grass communities. Rainfall manipulations treatments will be imposed for four years (2015 – 2018). Experimental plots are 4 x 4 m and hydrologically isolated. We passively alter rainfall reaching the plots by using a version of a hoop house rainfall reduction shelter (6 m x 9 m and 3 m tall). There are 6 replicates of each treatment (3 precipitation x 2 plant community; total of 36 plots).
Treatment effects on plant cover, composition, and physiology, as well as micrometeorological conditions are being measured. Plant cover, composition, and production are measured annually in spring and fall. Net photosynthesis and plant water status are measured monthly during the growing season. Plant phenology is measured by weekly. We have a complete meteorological station at the study site (data are available here) as well as micrometeorological stations measuring the effect of shelters on potential evapotranspiration. Soil moisture and temperature at two depths in each experimental plot is recorded by data logger.
We have numerous side studies taking place, including detailed root ecohydrologic investigations, in-depth studies on shrub ecology (Ephedra species), and others.
Future Directions
This is a relatively short-term, intensive experiment that we expect to provide valuable insights into the vulnerability of grassland ecosystems to extreme seasonal drought. Drought experiments of this scale are relatively rare—especially on the Colorado Plateau. We expect this study to provide valuable information on mitigating potential impacts of extreme drought on dryland ecosystems of the southwest US.
Below are other science projects associated with this project.
Ecohydrology and Climate Change in Drylands
Dryland Forest Sustainability
Aeolian Dust in Dryland Landscapes of the Western United States
RAMPS: Restoration Assessment & Monitoring Program for the Southwest
Chronic Drought Impacts on Colorado Plateau ecosystems (Rain-Out Experiment)
Big Sagebrush Ecosystem Response to Climate & Disturbance
Precipitation, soil moisture, and vegetation data from 36 experimental plots in southeastern Utah, near Canyonlands National Park (2015 - 2018)
Drought resistance and resilience: The role of soil moisture–plant interactions and legacies in a dryland ecosystem
Not all droughts are created equal: The impacts of interannual drought pattern and magnitude on grassland carbon cycling
Below are partners associated with this project.
- Overview
In drylands, short-term extreme droughts can have profound ecosystem effects, depending on the timing (seasonality) of drought and the sensitivities of the dominant plants and plant functional types. Past work suggests that cool season drought may disproportionately impact regionally important grass and shrub species. In this study, we are examining the impacts of extreme seasonal drought on grassland communities of the Colorado Plateau. This experiment was established in 2015 at one large site near Canyonlands National Park in southeastern Utah. We are focusing on the impacts of extreme (a 66% reduction in precipitation) warm and cool season drought on grass and mixed grass-shrub communities using large, moveable passive rainfall reduction shelters. This ongoing experiment is part of a larger network imposing extreme drought in grasslands globally (http://edge.biology.colostate.edu/).
Background & Importance
EDGE rainout shelter in a dryland ecosystem. (Credit: Michael Duniway, Southwest Biological Science Center. Public domain.) Drylands cover 41% of the terrestrial land surface and are one of the most vulnerable regions to changes precipitation and temperature. These arid and semiarid ecosystems are extremely resource limited, most notably for water, and thus any changes in water availability can lead to large ecological shifts. Like many drylands, the southwestern U.S. is experiencing warming and changes in precipitation. The early (2001-2010) was the warmest decade in in the instrumental record and models predict continued warming for this region. While periods of drought are a climatic feature of the southwest, recent “hot droughts” have had profound impacts on many southwest ecosystems. Grassland on the Colorado Plateau provide a myriad of important ecosystem services, including forage for livestock, habitat for wildlife, and conservation of soil resources. Thus, gaining new insights into drought vulnerabilities of Colorado Plateau grasslands is needed to mitigate deleterious impacts of future droughts.
General Methods
We are imposing extreme seasonal drought by excluding 66% of the natural precipitation using shelters that cover both grasses and shrubs. We have three precipitation treatments: 1) drought during the summer/fall growing season (May – October), 2) drought during the winter/spring cool season (November – April) and 3) ambient. We have applied each of these treatments to two different plant communities: 1) perennial grass community without shrubs and 2) mixed shrub-grass communities. Rainfall manipulations treatments will be imposed for four years (2015 – 2018). Experimental plots are 4 x 4 m and hydrologically isolated. We passively alter rainfall reaching the plots by using a version of a hoop house rainfall reduction shelter (6 m x 9 m and 3 m tall). There are 6 replicates of each treatment (3 precipitation x 2 plant community; total of 36 plots).
Treatment effects on plant cover, composition, and physiology, as well as micrometeorological conditions are being measured. Plant cover, composition, and production are measured annually in spring and fall. Net photosynthesis and plant water status are measured monthly during the growing season. Plant phenology is measured by weekly. We have a complete meteorological station at the study site (data are available here) as well as micrometeorological stations measuring the effect of shelters on potential evapotranspiration. Soil moisture and temperature at two depths in each experimental plot is recorded by data logger.
Collecting data on dryland plant community beneath EDGE rainout shelter. (Credit: David Hoover, USGS. Public domain.) We have numerous side studies taking place, including detailed root ecohydrologic investigations, in-depth studies on shrub ecology (Ephedra species), and others.
Future Directions
This is a relatively short-term, intensive experiment that we expect to provide valuable insights into the vulnerability of grassland ecosystems to extreme seasonal drought. Drought experiments of this scale are relatively rare—especially on the Colorado Plateau. We expect this study to provide valuable information on mitigating potential impacts of extreme drought on dryland ecosystems of the southwest US.
Field technicians collecting root data on dryland plant species. (Credit: David Hoover, USGS. Public domain.) - Science
Below are other science projects associated with this project.
Ecohydrology and Climate Change in Drylands
Drylands cover 40% of the global terrestrial surface and provide important ecosystem services. However, climate forecasts in most dryland regions, especially the southwest U.S., call for increasing aridity. Specifically, changing climate will alter soil water availability, which exerts dominant control over ecosystem structure and function in water-limited, dryland ecosystems. This research seeks...Dryland Forest Sustainability
Forests in the semiarid southwestern U.S. are expected to be highly vulnerable to increasing aridity anticipated with climate change. In particular, low elevation forests and the processes of tree regeneration and mortality are likely to be highly susceptible to climate change. This work seeks to characterize how, where and when forest ecosystems will change and identify management strategies to...Aeolian Dust in Dryland Landscapes of the Western United States
Dust emission caused by wind erosion has received considerable attention because of its far-reaching effects on ecosystems, including the loss of nutrients and water-holding capacity from source areas, changes to climate and global energy balance in areas where dust is entrained in the atmosphere, fertilization of terrestrial and marine ecosystems, in addition to decreases in snow albedo, causing...RAMPS: Restoration Assessment & Monitoring Program for the Southwest
The Restoration Assessment and Monitoring Program for the Southwest (RAMPS) seeks to assist U.S. Department of the Interior (DOI) and other land management agencies in developing successful techniques for improving land condition in dryland ecosystems of the southwestern United States. Invasion by non-native species, wildfire, drought, and other disturbances are growing rapidly in extent and...Chronic Drought Impacts on Colorado Plateau ecosystems (Rain-Out Experiment)
In drylands, chronic reductions in water availability (press-drought) through reduced precipitation and increased temperatures may have profound ecosystem effects, depending on the sensitivities of the dominant plants and plant functional types. In this study, we are examining the impacts of moderate, but long-term chronic drought using a network of 40 drought shelters on the Colorado Plateau...Big Sagebrush Ecosystem Response to Climate & Disturbance
Big sagebrush ecosystems are a major component of landscapes in the western U.S. and provide vital habitat to a wide array of wildlife species. However, big sagebrush ecosystems have been dramatically impacted by disturbances in the past several decades. This collaborative research between USGS and the University of Wyoming focuses on understanding how climatic and soil conditions influence big... - Data
Precipitation, soil moisture, and vegetation data from 36 experimental plots in southeastern Utah, near Canyonlands National Park (2015 - 2018)
These data were compiled for a study that investigated the effects of drought seasonality and plant community composition on two dominant perennial grasses, Achnatherum hymenoides (C3 photosynthesis), and Pleuraphis jamesii (C4 photosynthesis), in a dryland ecosystem. In 2015 USGS Ecologists recorded vegetation and soil moisture data in 36 experimental plots which manipulated precipitation in two - Publications
Drought resistance and resilience: The role of soil moisture–plant interactions and legacies in a dryland ecosystem
In many regions of the world, climate change is projected to reduce water availability through changes in the hydrological cycle, including more frequent and intense droughts, as well as seasonal shifts in precipitation. In water-limited ecosystems, such as drylands, lower soil water availability may exceed the adaptive capacity of many organisms, leading to cascading ecological effects during (coAuthorsDave Hoover, Alix A. Pfennigwerth, Michael C. DuniwayNot all droughts are created equal: The impacts of interannual drought pattern and magnitude on grassland carbon cycling
Climate extremes, such as drought, may have immediate and potentially prolonged effects on carbon cycling. Grasslands store approximately one-third of all terrestrial carbon and may become carbon sources during droughts. However, the magnitude and duration of drought-induced disruptions to the carbon cycle, as well as the mechanisms responsible, remain poorly understood. Over the next century, gloAuthorsDavid L. Hoover, Brendan M. Rogers - Partners
Below are partners associated with this project.