These tabular data were compiled for/to monitor vegetation and biocrust cover in a never grazed grassland located in Canyonlands National Park. An objective, or objectives, of our study was to document potential changes in biocrust and vegetation cover and species composition as related to changes in land use and climate change. These data represent a timeseries of long-term vegetation and biocrust monitoring plots, dating from 1996 to 2021. These data were collected at/in Virginia Park, Needles District of Canyonlands National Park, Utah. These data were collected by the U.S. Geological Survey, Southwest Biological Research Center in coordination with the US National Park Service. Data were collected via field observations twice annually, once in the Spring (April-May) and once in fall (Sept.) starting in 1996. A weather station was established in 1998 which recorded hourly temperature and precipitation measurements on a portable data storage module which was switched out and downloaded approximately every 3 months. These data can be used to monitor long term trends and changes in vegetation in a rare, protected and never grazed grassland on the Colorado Plateau, and help with monitoring trends in similar dryland ecosystems.

These tabular data were compiled for/to monitor vegetation and biocrust cover in a never grazed grassland located in Canyonlands National Park. An objective, or objectives, of our study was to document potential changes in biocrust and vegetation cover and species composition as related to changes in land use and climate change. These data represent a timeseries of long-term vegetation and biocrust monitoring plots, dating from 1996 to 2021. These data were collected at/in Virginia Park, Needles District of Canyonlands National Park, Utah. These data were collected by the U.S. Geological Survey, Southwest Biological Research Center in coordination with the US National Park Service. Data were collected via field observations twice annually, once in the Spring (April-May) and once in fall (Sept.) starting in 1996. A weather station was established in 1998 which recorded hourly temperature and precipitation measurements on a portable data storage module which was switched out and downloaded approximately every 3 months. These data can be used to monitor long term trends and changes in vegetation in a rare, protected and never grazed grassland on the Colorado Plateau, and help with monitoring trends in similar dryland ecosystems.

These data were compiled to investigate differentiation in physiological activity varies through time for different functional groups. These include the seasonal progress of 13 plant species representing perennial C3 shrub, C3 grass, C4 grass, and annual forb functional groups of the Colorado Plateau, USA. These data can be used to test for differences in carbon assimilation strategies (EcophyAciData) and how photosynthetic rates related to climate (EcophyMonthlyData). Data can be arranged at the seasonal, annual, species-, or functional group-levels to compare multi-level processes.

These data were compiled to investigate differentiation in physiological activity varies through time for different functional groups. These include the seasonal progress of 13 plant species representing perennial C3 shrub, C3 grass, C4 grass, and annual forb functional groups of the Colorado Plateau, USA. These data can be used to test for differences in carbon assimilation strategies (EcophyAciData) and how photosynthetic rates related to climate (EcophyMonthlyData). Data can be arranged at the seasonal, annual, species-, or functional group-levels to compare multi-level processes.

These data were compiled to examine how climate change affects biocrust recovery from both physical and climate-induced disturbance. Objective(s) of our study were to uncover the trajectory of biological soil crust communities and soil stability following distrubance and under warming. These data represent biological soil crust surveys under 5 treatments at three sites. These data were collected at three sites: Arches National Park, Canyonlands National Park and Castle Valley. Data collection for a physical disturbance experiment where annual human-trampling occurred at the sites in Arches and Canyonlands began in 1996 and was concluded in 2018. Data collection for a 13-year full-factorial in situ climate manipulation experiment (undisturbed control, warming, altered precipitation, warming + altered precipitation) in Castle Valley began in 2005 and was concluded in 2018. These data were collected by U.S. Geological Survey technicians using field surveys of biological soil crusts and soil stability. These data can be used to track biological soil crust communities and soil stability through time under climate manipulation and physical disturbance treatments.

These data were compiled to examine how climate change affects biocrust recovery from both physical and climate-induced disturbance. Objective(s) of our study were to uncover the trajectory of biological soil crust communities and soil stability following distrubance and under warming. These data represent biological soil crust surveys under 5 treatments at three sites. These data were collected at three sites: Arches National Park, Canyonlands National Park and Castle Valley. Data collection for a physical disturbance experiment where annual human-trampling occurred at the sites in Arches and Canyonlands began in 1996 and was concluded in 2018. Data collection for a 13-year full-factorial in situ climate manipulation experiment (undisturbed control, warming, altered precipitation, warming + altered precipitation) in Castle Valley began in 2005 and was concluded in 2018. These data were collected by U.S. Geological Survey technicians using field surveys of biological soil crusts and soil stability. These data can be used to track biological soil crust communities and soil stability through time under climate manipulation and physical disturbance treatments.

These data were compiled to assess the recovery of vegetation on reclaimed oil and gas sites. Objective(s) of our study were to assess patterns in reclamation outcomes relative to 1) soil attributes, climate, and time since 39 reclamation and 2) plant and soil reference benchmarks. These data represent observations of vegetation and soil cover from 134 reclaimed oil and gas well pads and 583 AIM reference plots. These data were collected on lands impacted by oil and gas development on the Colorado Plateau as well as Arizona and New Mexico Plateau of New Mexico, Colorado, and Utah. Data was collected from July- September of 2020 and May-September of 2021. These data were collected by Assessment Inventory and Monitoring (AIM) certified field crews using field observations and AIM methods. These data can be used to estimate plant community recovery on reclaimed oil and gas pads.

These data were compiled to assess the recovery of vegetation on reclaimed oil and gas sites. Objective(s) of our study were to assess patterns in reclamation outcomes relative to 1) soil attributes, climate, and time since 39 reclamation and 2) plant and soil reference benchmarks. These data represent observations of vegetation and soil cover from 134 reclaimed oil and gas well pads and 583 AIM reference plots. These data were collected on lands impacted by oil and gas development on the Colorado Plateau as well as Arizona and New Mexico Plateau of New Mexico, Colorado, and Utah. Data was collected from July- September of 2020 and May-September of 2021. These data were collected by Assessment Inventory and Monitoring (AIM) certified field crews using field observations and AIM methods. These data can be used to estimate plant community recovery on reclaimed oil and gas pads.

These data are daily climate, water balance, and soil moisture data for 270 plots in the National Park Service (NPS) Southern Colorado Plateau Network (SCPN) Inventory & Monitoring (I&M) network. Climate data was collected from a gridded, daily climate dataset, Daymet (https://daymet.ornl.gov/). Climate, alongside field-collected soils (SoilDepthsByPlot.csv) and vegetation information, were then used to drive a point based, daily, multi soil-layer, ecosystem water-balance model, SOILWAT2 (https://github.com/DrylandEcology/SOILWAT2). SCPN plots were established to capture the range of ecosystem conditions present in this network. Plant communities of the SCPN are a vital sign for this region, enhancing habitat, stabilizing soils, and moderating hydrology. However, these ecosystems are water-limited, and many plant and ecosystem processes are driven by the amount of water available in the soil profile (i.e. soil moisture). These data provide daily observations of gridded climate and predicted measures of water-balance (ie. transpiration, evaporation, etc.) and soil moisture availability for the last 38 years for 270 NPS plots and can be used to provide insight into plant and ecosystem processes.