Natural Notes National Park Service
U.S. Department of the Interior


2005

North Cascades National Park
Service Complex
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Eldorado Peak, by Tim Manns
Eldorado Peak. Photo: Tim Manns


Overview
Threatened Species
Forest Life
Aquatic Life & Science
Plant Ecology
Gelogy, Air & Climate
Cultural Resources
Glacier Monitoring
Citizen Science & What's Next?

NATURAL NOTES
National Park Service
U.S. Department of the Interior
North Cascades National Park Service Complex

NPS logo
Wiley Lake

Wiley Lake, North Cascades National Park

GLACIER MONITORING

Glaciers Mirror Global Climate Change

The North Cascades ecosystem has the highest concentration of glaciers in the lower 48 states. Studying climate response and changes in glaciers can help predict future climate changes. Since they are important to the health of the region and sensitive to fluctuations in climate, monitoring their status is a priority.

Over 700 of these slow moving giants, formed of rock and ice, play a critical role in natural processes and life of the entire region. At Thunder Creek in North Cascades National Park, glaciers contribute as much as 47% to total summer runoff.

The National Park Service began monitoring glaciers in North Cascades National Park in 1993 and in Mount Rainier National Park in 2002. The partnership between parks and the United States Geological Survey, which also monitors glacial trends, allows data to shed light on the global implications of climate change.

In North Cascades National Park, researchers Jon Riedel and Rob Burrows lead the monitoring of four glaciers that are at the headwaters of watersheds containing hydroelectric operations. Silver Glacier, which drains into Ross Lake, and Sandalee Glacier, which drains into the Bridge Creek watershed, are both east of the park's hydrologic crest. Noisy Creek Glacier, which drains into Baker Lake, and North Klawatti Glacier, which drains into the Thunder Creek watershed, are both on the west-side.

To gauge the dynamics of these glaciers, researchers use stakes to measure snow accumulation, radar to estimate thickness and aerial photos to study boundaries. Mass balances are the net amount of gain or loss glaciers experience each year. Current findings show a varied trend toward diminishing glacial mass balances. Glaciers east of the crest have not shrunk as quickly as their west-side counterparts in the first decade of study. Reasons for the differences might include higher elevations and more northerly aspects of the east-side glaciers.

Besides telling us about the health of these glaciers, the studies show how glacial runoff contributes to watersheds and regional ecology. This year, a 10-year data summary will be published on this ongoing research.

www.nps.gov/noca/massbalance.htm