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Loch Vale Long Term Ecological Research Program: Celebrating Stewardship and Science Since 1982

Sky Pond
Sky Pond, an alpine lake in the Loch Vale Watershed.

NPS Photo

The Loch Vale Watershed is a glacially carved, high-elevation catchment and long-term ecological research site in the Bear Lake Corridor of Rocky Mountain National Park (RMNP). The watershed spans alpine and subalpine ecosystems and includes alpine lakes, glaciers, subalpine forests, and wetlands. For researchers, Loch Vale offers a comprehensive look at watershed-scale ecological processes and how global change effects high-elevation ecosystems.

Initial research in Loch Vale was conducted by the U.S. Geological Survey (USGS) and focused on the ecological effects of acidic atmospheric deposition (acid rain) to soils, plants, and lakes. Since then, collaboration between USGS, Colorado State University (CSU), and the National Park Service (NPS) has expanded research to explore the ecological consequences of nitrogen deposition, carbon cycling, and the effects of climate change. Within each field, researchers strive to disentangle natural processes from human-caused drivers of change.

Explore Data Here

Myriad long-term, open-source datasets are available for the Loch Vale Watershed thanks to efforts by USGS and CSU. These datasets include atmospheric deposition chemistry, streamflow, stream and lake chemistry and biology, weather, and plant species lists. Long-term datasets and monitoring efforts are essential to understanding change over time, as they provide continual data and baseline conditions for which to compare.
 

Rocky Mountain National Park

Last updated: February 8, 2024