New Weather Stations Aid Denali Researchers and Climbers

New weather stations provide live updates of conditions on Alaska’s Denali, the tallest peak in North America. The weather stations sit atop the mountain on the Kahiltna Glacier and provide important weather information for climbers and scientists alike. They allow scientists to track snowpack and provide the climbing community with a better sense of weather conditions on the 20,310 foot mountain.

Michael Loso, a National Park Service geologist, started the project in order to better understand weather patterns at higher altitudes. GlacierHub spoke with Loso to get a better understanding of the project and its impacts.

GlacierHub: How do these new weather stations on Denali help climbers and help researchers assess glacial retreat?

Mike Loso: We’ve established three new weather stations in the accumulation zone of Denali’s Kahiltna Glacier. These stations, at approximately 7,000, 10,000, and 14,000 feet, continuously measure air temperature and snow accumulation and melt on a year-round basis. In addition, the highest and lowest stations measure wind speed and direction, incoming and outgoing solar radiation, and send those measures via satellite telemetry back to publicly available servers on a continuous basis. They provide critical information for mountaineers, for weather forecasters, and for National Park Service climbing/rescue rangers. The fact that two of these stations are providing regular, real-time, hourly, year-round weather information means that climbers can plan their trips wisely.

Glaciologists like me use the data from these stations to understand the year-round patterns of snow accumulation and melt, and to compare those measurements with existing measurements we have been making for decades at lower elevation sites on the Kahiltna. Together, all these measurements allow us to measure not only the net shrinkage of Kahiltna Glacier, which is ongoing, but more importantly to understand how that shrinkage is controlled by the detailed changes in our climate.

GH: How are these measurements different than how researchers typically observe a glacier’s status?

ML: Most glacier mass-balance studies have traditionally focused on glaciers that are fairly small, or in the cases of larger, higher-elevation glaciers they favor measurements in the lower elevations. There are very few studies of snow accumulation and melt at high elevations of large glaciers because it is too difficult to install and maintain on-glacier weather stations in such inhospitable environments. But those high elevation sites are usually the very places where most snow accumulation occurs, even in the summertime during what would be considered the “melt season” at lower elevations. So glaciologists still have uncertainty about year-round patterns of snow accumulation, and the only way to measure that is to measure it continuously. But that’s difficult. If you place the weather station on a rocky outcrop near the glacier, then you are definitely not getting a “true” signal of snow accumulation because rocky outcrops are by definition wind-scoured and atypical of the glacier’s accumulation zone. If you place a normal weather station on the glacier itself, it will promptly get buried by ongoing snow accumulation. So our strategy is to place the stations on very tall masts that are anchored in the glacier surface and then to periodically dig the stations out and “reset” them when the snow threatens to bury the existing station. We couldn’t accomplish this without a lot of logistical support, and that is possible on Denali only because of the substantial operation run by the National Park Service mountaineering rangers. They establish and maintain rescue camps at 7,000 and 14,000 feet on the Kahiltna Glacier, and their presence (along with the aviation assets required to support that operation) allow us, in partnership with them, to maintain these stations.

GH: What makes the Denali glacier unique in terms of climate change?

ML: Denali is the tallest mountain in North America, and it is located in a fairly high latitude, by US standards. So the top is a really cold place, even by the standards of most glaciers. That cold (and windy) climate results in patterns of snow accumulation and snow and ice melt that are not typical of most glaciers in the US. typically glaciers accumulate more snow as you go higher with maximum accumulation near the summit. But anecdotal observations suggest that this pattern does not apply at Denali. Instead, it appears that snow accumulation is actually highest at the mid-elevations of the Kahiltna Glacier and that snowfall diminishes as you go higher. That’s unusual, and is probably due in part to the inability of very cold air to hold much moisture. Interestingly, some of our colleagues recently published findings that snow accumulation rates on nearby Mount Hunter appear to have actually increased over recent centuries. We hypothesize that some of that increase may be due to the enhanced ability of warmer air to hold and then release moisture—a process that might lead to more snowfall on the Kahiltna Glacier as climatic warming continues. Our data will allow us to test this intriguing hypothesis.

GH: Are there any other parks that are using these types of weather stations

ML: Some of the technology (sensors, power supply, data-loggers) are in common use, but this particular application in a high-glacier, snow-accumulation environment is not presently being done anywhere else that we’re aware of. That said, similar designs have been applied sporadically in the past, and we have benefitted from lessons learned during those experiences.

Scientists Pam Sousanes, Dom Winski, and Michael Loso program a Denali weather station. (Source: National Park Service/Tucker Chenoweth)

GH: What inspired the project?

ML: In addition to the desire to understand glacier environments better, to better predict mountain weather, and to provide real-time information for climbers and rescue rangers, I was especially motivated to tackle this project by my own history on Denali. Fresh out of college I worked for a couple seasons as both a guide and a mountaineering ranger on Denali, and then over the subsequent 20 plus years I’ve stayed involved there as a volunteer rescue patrol member, as a scientist, and as a recreational skier and climber. Through those experiences, I’ve come to know the mountain well, but also many of the long-term professionals working on the mountain (guides, rangers, pilots). So I’ve come to really love the place and to have a fairly broad knowledge of the scientific and societal challenges posed there by climate change. In light of all that, this project really excited me and continues to be a pleasure to work on.

GH: What does the future look like for this technology?

ML: The technology itself is not anything unusual. We are just deploying that technology in a somewhat unusual way and place. I would call our work experimental, in the sense that we expect to see challenges and damages related to the extreme climate. But as we learn from those failures, I would expect that we will capitalize on opportunities to apply this technique in other places.

Read More on GlacierHub:

UNESCO-Recognized Glaciers Could Shrink 60 Percent by End of Century

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GlacierHub Seeks Contributors for Its New, International Feature Series

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Photo Friday: A look at the 2017 Denali Mountaineering Season

It’s summer in Alaska, and for some intrepid adventurers, that means it’s mountaineering season on Denali, the iconic peak whose name means “The High One” in the Koyukon Athabascan language. According to the Denali National Park Service mountaineering blog, Denali Dispatches, there are currently 520 climbers attempting the highest peak in North America. 142 climbers have already reached the summit this season, a 34 percent success rate.

This week held some excitement for the Park Service, which on June 5th responded to two simultaneous medical incidents on the Kahiltna Glacier. One climber, suffering from “acute abdominal illness,” was assessed and helped by park personnel to Kahiltna Glacier Base Camp. More dramatically, another climber was un-roped when he fell forty feet into a crevasse on the West Buttress route, and became wedged in the ice. Rangers arrived at the accident site at 4 a.m., and after nearly twelve hours of chipping away ice with power tools, they were finally able to extract the injured and hypothermic climber, who was hastily evacuated to the hospital in Fairbanks.

 

Rangers camp above the toe of the Ruth Glacier (Source: Dan Corn/NPS).

 

Looking down the Kahiltna Glacier. A heavily crevassed area is visible in the lower left of the photo (Source: Tucker Chenoweth/NPS).

 

Park Service personnel practice crevasse rescue skills near Kahiltna Basecamp (Source: Steve Mock/NPS).

 

Bundled-up climbers watch the small planes that bring people to and from Kahiltna Basecamp (Source: Steve Mock/NPS).

 

Low winter snow pack and cold spring temperatures create weak, sagging snow bridges over crevasses, which are seen as stripes outside this camp on Denali (Source: NPS).

 

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Photo Friday: The Glacial Alaska Range

The Alaska Range is a narrow, 700-kilometer mountain range defined by rugged peaks and large U-shaped glacial valleys. The range lies in the southeast corridor of Alaska and is home to Denali, the tallest peak in North America. The Alaska range is part of the American Cordillera and possesses peaks only trumped by those in the Himalayas and Andes.

For many decades, the Alaska Range has played host to an incredible variety of landscapes and ecology, with visitors traveling from all over the world to hike, climb and sight see in Denali National Park. One-sixth of Denali National Park, or approximately one million acres, is covered by glaciers, which transport thousands of tons of ice each year, according to the National Park Service. Take a look at GlacierHub’s collection of images of Alaska’s impressive peaks and low valleys shaped by glacial activity over the past million years.

 

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An aerial view of the high altitude peaks of the Alaska Range (Source: Matt Verso/Creative Commons).

 

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Road entering Denali National Park on the east edge of the Alaska Range (Source: Arthur Chapman/Creative Commons).

 

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The U.S. Army flies a helicopter toward Kahiltna Glacier, the longest glacier in the Alaska Range (Source: Defense.gov/Creative Commons).

 

Moving toward the Harper Glacier in Denali National Park (Source: Mikep/Creative Commons).
Moving toward the Harper Glacier in Denali National Park (Source: Mikep/Creative Commons).

 

An aerial view of the Upper Muldrow Glacier, Denali National Park (Source: Pete Klosterman/Creative Commons).
An aerial view of the Upper Muldrow Glacier, Denali National Park (Source: Pete Klosterman/Creative Commons).

 

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Looking south across the Monahan Flat (Source: Albert Herring/Creative Commons).

 

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Looking east across the Monahan Flat (Source: Paxon Woelber/Creative Commons).

 

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Southern edge of the Alaska Range (Source: Denali National Park/Creative Commons).

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