Photo Friday: A Look at Wolverine Glacier

Wolverine Glacier is a valley glacier with maritime climate and high precipitation rates situated in the coastal mountains of Alaska’s Kenai Peninsula. This glacier has been named a “reference glacier” by the World Glacier Monitoring Service because it has been monitored and observed since 1965/66. A majority of the U.S. government’s climate research is taken from 50 years of glacier studies from the United States Geological Survey (USGS). Scientists first decided to take measurements of Wolverine Glacier’s surface mass balance in 1966, using these measurements, as well as local meteorology and runoff data, to estimate glacier-wide mass balances, according to USGS. This data, which makes up the longest continuous set of mass-balance data in North America, allows scientists to better understand glacier dynamics and hydrology, as well as the glaciers’ response to climate change.

As temperatures rise, the retreat of glaciers in Alaska is contributing to global sea-level rise. The Wolverine Glacier has been experiencing more variability in winter temperatures, and scientists are continuing to evaluate how glaciers like the Wolverine respond to climate change. Take a look at GlacierHub’s collection of images from Wolverine Glacier.

 

Scientists checking ablation stakes at Wolverine Glacier (Source: USGS).

 

A weather station set up to measure the spatial differences in climate that influence mass balance (Source: USGS).

 

Researchers use ground penetrating radar to determine the depth of the snow on Wolverine Glacier (Source: USGS).

 

The crevassed surface of Wolverine Glacier shows layers within the ice and snow (Source: USGS).

 

Photo Friday: Benchmark Glaciers in the USA

Glaciers contain about three quarters of the world’s fresh water and cover about 75,000 square kilometers of the U.S. The United States Geological Service (USGS) has been running the Benchmark Glacier program since the late 1950s to track glacier mass balance. Repeat measurements at four selected sites are used in conjunction with local meteorological and runoff data to measure the glaciers’ response to climate change.

Results from South Cascade Glacier in Washington and Gulkana and Wolverine glaciers in Alaska provide the longest continuous record of North American glacier mass balance. In 2005, Sperry Glacier in Montana was added to the program, allowing changes in glacier mass in the principal North American climate zones to be tracked.

South Cascade Glacier in Washington experiences some of the highest precipitation levels in the lower 48 states of the USA, exceeding 4500mm per annum in some places. Data was first collected from this glacier in 1959.

 

South Cascade Glacier as seen in 1928 (left) and 2006 (right) (Source: USGS)
South Cascade Glacier as seen in 1928 (left) and 2006 (right) (Source: USGS).

 

A researcher collecting a snow core sample from South Cascade Glacier (Source: USGS)
A researcher collecting a snow core sample from South Cascade Glacier (Source: USGS).

 

Gulkana Glacier can be found along the southern flank of the eastern Alaska range. It experiences a continental climate, with large temperature ranges and precipitation that is more irregular and lighter than that experienced in coastal areas.

 

Gulkana Glacier and surrounding peaks (Source: USGS)
Gulkana Glacier and surrounding peaks (Source: USGS).

 

Northern lights over the researchers’ cabin in 2014 (Source: USGS)
Northern lights over the researchers’ cabin in 2014 (Source: USGS).

 

A researcher measuring the thickness of the snow at Gulkana glacier (Source: USGS)
A researcher measuring the thickness of the snow at Gulkana Glacier (Source: USGS).

 

Wolverine Glacier is also located in Alaska, but is found in the Kenai Mountains on the coast. The maritime climate has low temperature variability and regular, heavy precipitation. Data collection at both Gulkana and Wolverine glaciers began in 1966.

 

Wolverine Glacier in 2014 (Source: USGS)
Wolverine Glacier in 2014 (Source: USGS).

 

The weather station at the top of Wolverine Glacier (Source: USGS)
The weather station at the top of Wolverine Glacier in Alaska (Source: USGS).

 

The crevassed surface of Wolverine Glacier (Source: USGS)
The crevassed surface of Wolverine Glacier in the Kenai Mountains (Source: USGS).

 

Sperry Glacier is located in the Lewis Range of Glacier National Park in Montana. The climate of the region is influenced by both maritime and continental air masses, but Pacific storm systems dominate. These systems result in moderate temperatures and heavy precipitation, which vary strongly with altitude.

 

Sperry Glacier in 1913 (top) and 2008 (bottom) (Source: USGS)
Sperry Glacier in 1913 (top) and 2008 (bottom) (Source: USGS).

 

Researchers inserting ablation stakes using a steam drill (Source: USGS)
Researchers inserting ablation stakes using a steam drill (Source: USGS).