Effects of global change on alpine and subalpine ecosystems
Synthesizing a data legacy to provide scientific and management insight for Rocky Mountain National Park and beyond
Atmospheric nitrogen deposition, climate change and recreation are rapidly altering high elevation ecosystems. This project will evaluate long-term biogeochemical, hydrological, and ecological trends in Rocky Mountain National Park to understand the causes and rates of change in alpine and subalpine waters, soils, and vegetation. Policy makers and resource managers of high-elevation, protected lands can use the resulting knowledge to better protect these ecosystems.
Statement of Problem
The independent and interactive effects of climate change and atmospheric nitrogen deposition are rapidly altering mountain ecosystems worldwide. Changes that began in the mid-20th century are continuing and accelerating today, altering ecosystem processes and species assemblages, especially in high elevation lakes, forests and the alpine tundra. Resource managers and policy makers have been using our research and monitoring data on Rocky Mountain National Park’s alpine and subalpine lakes since 1983. Now that we have over forty years of data, we need to synthesize ecosystem change patterns and processes across decades to distinguish natural from human-caused changes, and identify potential tipping points in chemistry and climate that may harm these iconic landscapes. The results will be shared with our collaborators to create or alter management and policy activities that can protect and restore mountain ecosystems in a changing world.
Why this Research is Important
Scientists, resource managers, and policymakers can use this synthesis to project future ecosystem behavior. Our findings will also inform the broader scientific community about how high elevation ecosystems may change. We plan to compare site-specific results to other high elevation locations to build a larger understanding of pattern shifts across high elevation ecosystems. Finally, we will work with resource managers to apply findings for framing resist-accept-direct (RAD) and similar management actions.
Objective
Synthesize more than 40 years of research and monitoring information of the alpine-subalpine Loch Vale watershed in Rocky Mountain National Park.
Methods
We will use a combination of data science, ecosystem ecology, biogeochemical insights, statistics and remote sensing. The comprehensive approach will be used to identify past, present, and projected future patterns of biogeochemical and ecological change and their causes. Results will be shared with our NPS partners and with the broader scientific community.
Interpreting Global Change Impacts on Southern Rocky Mountain Alpine and Subalpine Ecosystems for Effective Resource Management
Accelerating changes and transformations in western mountain lakes
The Western Mountain Initiative (WMI)
Western Mountain Initiative: Central Rocky Mountains
Western Mountain Initiative: Colorado
Soil and surface water nitrogen and caffeine data from 2019, and 2019-2020 trail counts of hikers in Loch Vale Watershed, Rocky Mountain National Park
Climatological data for the Loch Vale watershed in Rocky Mountain National Park, Colorado, water years 1992-2019
Water chemistry and land cover attributes for The Loch and Sky Pond, Rocky Mountain National Park
Paleoecological data from The Loch and Sky Pond, Rocky Mountain National Park
Climatic variability as a principal driver of primary production in the southernmost subalpine Rocky Mountain lake
Proximity to roads does not modify inorganic nitrogen deposition in a topographically complex, high traffic, subalpine forest
Warming-induced changes in benthic redox as a potential driver of increasing benthic algal blooms in high-elevation lakes
Marmots do not drink coffee: Human urine contributions to the nitrogen budget of a popular national park destination
Identifying factors that affect mountain lake sensitivity to atmospheric nitrogen deposition across multiple scales
Persistent nitrate in alpine waters with changing atmospheric deposition and warming trends
Long-term ecosystem and biogeochemical research in Loch Vale watershed, Rocky Mountain National Park, Colorado
Nutrients and warming alter mountain lake benthic algal structure and function
Nutrients and warming interact to force mountain lakes into unprecedented ecological state
2017 Monitoring and tracking wet nitrogen deposition at Rocky Mountain National Park
Reducing wet ammonium deposition in Rocky Mountain National Park: The development and evaluation of a pilot early warning system for agricultural operations in eastern Colorado
Long-term nitrogen addition shifts the soil nematode community to bacterivore-dominated and reduces its ecological maturity in a subalpine forest
Atmospheric nitrogen deposition, climate change and recreation are rapidly altering high elevation ecosystems. This project will evaluate long-term biogeochemical, hydrological, and ecological trends in Rocky Mountain National Park to understand the causes and rates of change in alpine and subalpine waters, soils, and vegetation. Policy makers and resource managers of high-elevation, protected lands can use the resulting knowledge to better protect these ecosystems.
Statement of Problem
The independent and interactive effects of climate change and atmospheric nitrogen deposition are rapidly altering mountain ecosystems worldwide. Changes that began in the mid-20th century are continuing and accelerating today, altering ecosystem processes and species assemblages, especially in high elevation lakes, forests and the alpine tundra. Resource managers and policy makers have been using our research and monitoring data on Rocky Mountain National Park’s alpine and subalpine lakes since 1983. Now that we have over forty years of data, we need to synthesize ecosystem change patterns and processes across decades to distinguish natural from human-caused changes, and identify potential tipping points in chemistry and climate that may harm these iconic landscapes. The results will be shared with our collaborators to create or alter management and policy activities that can protect and restore mountain ecosystems in a changing world.
Why this Research is Important
Scientists, resource managers, and policymakers can use this synthesis to project future ecosystem behavior. Our findings will also inform the broader scientific community about how high elevation ecosystems may change. We plan to compare site-specific results to other high elevation locations to build a larger understanding of pattern shifts across high elevation ecosystems. Finally, we will work with resource managers to apply findings for framing resist-accept-direct (RAD) and similar management actions.
Objective
Synthesize more than 40 years of research and monitoring information of the alpine-subalpine Loch Vale watershed in Rocky Mountain National Park.
Methods
We will use a combination of data science, ecosystem ecology, biogeochemical insights, statistics and remote sensing. The comprehensive approach will be used to identify past, present, and projected future patterns of biogeochemical and ecological change and their causes. Results will be shared with our NPS partners and with the broader scientific community.