Tag: glacier

Preservation Of North Cascade Glaciers

On By mspeltoIn climate change glacier retreat, glacier climate change

Recipe for Mountain Glacier Formation:

Recent glacier thinning due primarily to warm summers has exposed new bedrock knobs on upper portions of Deming, Easton and Squak Glacier on Mounty Baker, Washington

Find a location where temperatures are cold for at least 7 months of the year. This location also needs to have substantial snowfall and ideally where addtiional snow is added via avalanches or wind depostion. With these ingredients on hand, let stand for a few decades, while the snow accumulates to a thickness of at least 20 m. A key step in the recipe is the transformation of snow to ice under its own weight and with some meltwater percoloation and refreezing. Unlike bread dough you do not need stir or kneed during this period. Once there is a volume . For the glacier to persist the glacier must retain accumulation across a significant portion of its surface by the end of summer. To maintain its size we have observed this percentage to vary from 50-70% on North Cascade glaciers. The lack of a persistent accumulation zone will lead to loss of that glacier. of 500,000 m3 you are either a glacier or at the threshold of being a glacier depending on how steep the underlying slope is. Unlike rolling out a pie crust, this does not need to be an even thickness, or made on a flat surface. As the glacier matures it will develop crevasses indicating movement, which is an essential characteristic of a glacier. It is not a passive feature, its movement allows it to begin to sculpt its landscape.

Current Glacier Loss in North Cascade Range, Washington

Many centuries or millenia later, the glacier has become a critical part of the landscape. Yet, changing climate is leading to the loss of many. In the North Cascades glaciers have been losing close to 1% of their volume annually over the last 40 years, with the rate rising to over 2% in the last decade. The glaciers cover 200 km2 almost all of which are in steep high elevation Wilderness areas not proximate to roads. In 2010 we noted that 2/3 of North Cascade glaciers could not survive current climate. Today this percentage has increased to more than 90%. There are 31 glaciers in the range that I completed observations on in the 1980s that are now gone. Our annual field expedition has noted the glaciers losing ~1.5 m of thickness annually in the last decade.

Deglaciated area below Easton Glacier, Mount Baker, WA in 2023.

Are there any Preservatives we can add to the Recipe?

What would it take to preserve the Easton Glacier in the North Cascades? 

The largest snowmaking operation in North America is at Killington Ski Area, VT. At maximum capacity they can convert 35,000 m3 of water into snow per day. Given that Easton Glacier has an area of 2.5 km2 and has been losing 1.5 m water equivalent thickness per year, 3.75 million m3 of water equivalent snow has to be produced.This would take 108 days at maximum capacity of the more than 2000 snow guns. This ignores enviornmental laws and the logistics of water supply, piping, snow gun placement and electricity. This all in an environment of harsh weather with avalanches and crevasses.

Killington, Vermont snowmaking operation.

To cover the glacier with geotextiles during the summer, requires 2.5 million square meter of material that would be to installed each summer and removed each winter to allow accumulation, of course summer recreation would not be practical on the glacier. The geotextiles do not last long in these conditions and cost ~$2 per square meter. How to anchor these in place and connect on a crevasse glacier would be very difficult, which is why usually only a portion of the glacier near the terminus is covered, which does not help the overall situation of glacier loss.

Tarps at top of Gurschen Glacier, Switzerland, that reduce the melt locally note groomer for scale.

There are many more glaciers in this range and around the world where this same confounding logistical challenges make any artificial attempts at preservation ridiculous beyond a few isolated glaciers that are already close to existing infrastructure.

When I began this work in 1984 solar power and wind power did not exist, these are not the only renewable sources of power, and just one of many approaches to reducing CO2 emissions, but they are illustrative of rapid growth from insignificance. The Renewalbes 2014 Global Status Report and the Renewables 2024 Global Status Reports provides measures of renewaable energy production over the last decade. Global capacity for Solar Photovoltaic energy production has risen from 4 GW in 2004 to 190 GW in 2014 and then to 1600 GW in 2023. Global Capacity for Windpower has risen from 48 GW in 2004 to 370 GW in 2014 and in 2023 was 1020 GW. In 2023 alone over 500 GW was added to these two sources combined. See below for charts from this report on increased capacity. This is a preservative under development that can work with continued emphasis and in concert with other items such power grid infrastructure improvement and electric/hybrid automobile manufacturing expansion.

Himalayan Glacier Snow Lines High and Rising November 2024

On By mspeltoIn Glacier Observations, Himalaya glacier retreat
Mount Everest Region, Nepal glacier snow lines on Sentinel image from 11-12-2024. Mean elevation of snow lines is 5800 m.

As the post-monsoon period progresses, glacier snow lines have been rising in the Himalaya. Will this be similar to last year and in 2020/21 when the snow line on many glaciers remained high right through much of the winter? Here we examine Sentinel 2 imagery from Kanchenjunga Glacier on the eastern border of Nepal to the Gangotri Glacier in Uttarakhand, India. In November snow lines are averaging from 5500 m to 6000 m (yellow dots are snowline). In each location there is clear upward shift of the snow line since the beginning of October, 2024.

The rising snow lines indicate significant ablation is occurring at least up to that point. There has been a trend in the last decade where ablation conditions are extending into the winter season most years (Pelto et al 2022). Will the winter 2024/25 follow this trend?.

Kanchenjunga Glacier with the November 17, 2024 snow line averaging 6000 m.
Langtang Glacier, Nepal with the snow line on November, 17 2024 averaging 5500 m.
Gangotri, Satopanth and Bhagirath Kharak Glacier snow line on Sentinel 2 image from 11-06-2024. Mean elevation is 5500 m.

Reflections from the 2024 North Cascade Glacier Climate Project Field Season

On By mspeltoIn Glacier Observations, North Cascade Glaciers

The 2024 field season was our 41st, from the glaciers perspective it was the fourth consecutive year of exceptional mass loss, leading to thinning, retreat and glacier loss. Below are images from the field season and reflections on each from the varied perspectives of our field team and field partners.

Coleman Glacier, Mount Baker at the golden hour as we just finished work.

Jill Pelto: During the field season our typical day involves getting up with the sun and working out on a glacier until early evening. Going to Coleman Glacier on Mt. Baker this year was special because we got to work on it during golden hour, a rare thing to experience. We had the glacier to ourselves, and the nearby big camping area — despite this being a popular destination for ice climbers. This is only my third time in sixteen years working on this glacier, and its significant loss since we last saw it in 2019, when I sat and painted on it, was so apparent. But in spite of that, I was feeling joyful to be there — something about four of us out there on our own taking measurements as the summer sun set was so magical. I was so grateful to be there at that moment and experience this landscape as it is now. 

Saddle at top of Rainbow Glacier looking to summit of Kulshan (Mount Baker). Ben, Jill and Mauri Pelto a combined 70+ years of experience on these glaciers.

Mauri Pelto: Climate change has led to increased glacier melting on all of the glaciers we have observed. A combined 70+ years of field experience that Ben, Jill and I have provides a context that is crucial. The increased melt is apparent in the streams flowing across the surface very few meters carrying meltwater to the rivers and then the sea. This summer we saw the beauty of the final stages of decay of a glacier melting away in the ice caves that transected the former Ice Worm Glacier (image below). The cave started at the top of the glacier and continued right to the bottom, by next summer that too will be gone. The colors and atmosphere in the cave were spell binding. The landscape remains beautiful, but is losing the glaciers that are a powerful, beautiful and dynamic part of this landscape.

Katie Hovind: Nestled along Ptarmigan Ridge, overlooking Kulshan’s glacier-flanked slopes, was our longest campsite of the field season. Unzipping my tent to an increasingly familiar skyline four mornings in a row, I found myself developing a relationship with this place. I noticed patterns and changes alike, discovering not just the place but a sense of home in it. We followed transects across the Sholes, probing up and down the glacier; we explored a collapsed ice cave near its terminus, blue ice towering over me, ancient wisdom frozen in the dripping layers I ran my hands along; we took water measurements from the stream it feeds, pausing for a break next to the fresh melt as I sketched the textures of rock and snow and ice. We commuted across it twice to the Rainbow Glacier, a trek familiarizing me with the Sholes’ sweeping slopes and views; and we screwed an ice auger deeper than we could see, dropping stakes 3-4 feet below the surface. 19 days later, I returned to the coordinates of those four stakes, which were now all exposed, one sticking up to just over 3 feet above the surface. Reeling as I walked across the glacier I’d gotten to know, the near-incomprehensible volume of loss I saw. A feeling of belonging is so integral to caring. And then comes the question of how to transmit that connection, to spread to others the same sense of responsibility to protect a place? Being lucky enough to experience even a handful of days taking in just a small degree of the Sholes’ nuances, I felt deeply just how wrong and quick the melt is. But from the outside looking in, without any prior reference points, the severity of the glacier shrinking could be overlooked. Through these comparison photos, I hope to share just a glimpse, beauty and grief and all, of what it means to understand and love a glacier.

Emma Murray: Just a few minutes into our hike from camp to the Easton glacier, Science Director Mauri Pelto pointed out the rock that marked the spot where he put his crampons on in 1990. Looking up the valley, the ice felt SO far away. This glacier has retreated almost 600m in my lifetime already. In response to the melting at each of the six glaciers I visited during my time with the Project, I added paint, pen, and thread to canvas. These flags are both white-flag surrenders to all the melting we cannot stop and blowing-in-the-wind prayers for us all to act in the ways we can. I hope these pieces help people to visualize and feel the difference between where the ice was and where it is now. I think feeling that loss is groundwork for our urgent conversations about climate solutions, which can be uplifting and cool and pragmatic and creative!

Shari Macy: Mauri Pelto, peers into the melting terminus of the Lower Curtis Glacier; located on the southern slopes of Mount Shuksan in the North Cascades of Washington State. As founder of the North Cascade Glacier Climate Project, he has been measuring these shrinking giants since 1984. This image, to me, shows a man and what he dedicated his life to studying. A passion that drove him to spend over 700 nights in tents, camped out next to the glaciers of the North Cascades. These glaciers could use a lot more people like Mauri. Does everyone need to backpack to remote glaciers every summer? No. He already does. However, we could all be a little more dedicated to the health of our planet, our home. Our one and only. Our children’s one and only.

Megan Pelto: To me, Mt. Baker represents the North Cascades. Camping next to its looming presence makes me aware of how impactful it is, its glaciers helping support the ecosystem and the wildlife that surround it. Getting to be present in this wilderness feels like a gift and a chance to both disconnect and reconnect. Everything you have is contained in one little tent and the experience of camping in this landscape is magical. I wanted to capture that with our colorful little tents tucked into grassy hills with Baker above us. I have been able to visit this landscape over the past 10 years, and while the glaciers change each year, many things have remained peacefully the same.

Ben Pelto: Disappearing glaciers remind me of grandparents—I’m saddened by their decline, yet deeply grateful for the time I still have with them. This year, being in the field was especially meaningful, surrounded by an incredible group of people, just experiencing the mountains and soaking it all in. What I find hardest about glaciers vanishing is not just the loss of ice, but the disappearance of their dynamism and beauty from the landscape. These ancient giants bring a sense of magic and power to the mountains, and it breaks my heart to think that my children or grandchildren might never witness them as I have.

Cal Waichler: This season I ask what it means to be a voice for glaciers. How can I transmit my gratitude that I can stand on this earth, breathe glaciers’ breezes, seep in icy blue and alpenglow rose, pop alpine huckleberries in my mouth, and notice the shrinking snow and dissolving ice, while also alerting people to their vulnerabilities? Glaciers are a throughline in my explorations and art. I am so utterly enchanted by them. The awe and creative inspiration they bring to my life is a great gift. As a voice for shrinking glaciers, what stories can I share that will enchant other people with them? What will make us care enough to enact climate change mitigation and adaptation, and vote for climate leaders? Here, a snapshot of those most transient and irreplaceable things.

Mount Everest Glaciers Limited Snow Cover Persists From November 2023 into May 2024

On By mspeltoIn Glacier Observations
The snow line on Mount Everest Region glaciers on May 1,, 2024 indicated by yellow dots on the Landsat image. Note that Nangpa La and Nup La-two high passes (5800-5900 m) are both snow free. The average snow line is 6050 m.

This is a update to a previous post examining high snow lines through the winter on Mount Everest Region glaciers. Here we examine imagery from October 2023 through early May 2024 illustrating the rise in snow line into January and the continue high elevation into the pre-monsoon season. The persistent high snow line over the last six months, indicates a lack of snow accumulation during the winter season. This is a dry season, yet typically leads to extensive, though not particularly deep snow cover. There were a few smaller snow events, but the snow cover did not persist indicating that ablation has continued even above 6000 m on Mount Everest. The lack of snow leads to less infilling of crevasses on Khumbu Glacier, which are further opened by persistent ablation. On May 1 there is evident blue ice and firn areas in the Western Cwm, above the Khumbu Icefall and on the Lhotse Face above the Western Cwm at the head of the Khumbu Glacier. The relatively bare slopes above the Western Cwm also cannot generate as much avalanches that would then accumulate snow in that basin. These same slopes will yield more rock fall, with more exposed unburied rock.

In the Khumbu Icefall velocities indicates by NASA ITS LIVE are ~1m/day which leads to considerable crevasse development in the six months from November into May with very limited snow accumulation and evident ablation, image below. This season is different than the high snow lines i 2020/21 that resulted from extraordinary January heat wave. Snow cover did develop at the end of the winter/early spring (Pelto et al 2021).

The snow line on Khumbu Glacier on May 1,, 2024 indicated by yellow dots on the Landsat image. Note that there are bare ice areas in the Western Cwm (WC) and on the Lhotse Face (LF).
The snow line on Mount Everest Region glaciers on March 14, 2024 indicated by yellow dots on the Landsat image. Note that Nangpa La and Nup La-two high passes (5800-5900 m) are both snow free. The average snow line is 5950 m.

The snow line on Mount Everest Region glaciers on Feb. 11, 2024 indicated by yellow dots on the Landsat image. Note that Nangpa La and Nup La-two high passes (5800-5900 m) are both snow free. The average snow line is 6000 m.

The snow line on Mount Everest Region glaciers on Jan. 10, 2024 indicated by yellow dots on the Landsat image. Note that Nangpa La and Nup La-two high passes are both snow free. The average snow line is 5950 m
Khumbu Glacier on Feb. 11, 2024 in Landsat image illustrating snow line near top of icefall at 6000 m, yellow dots. There is some blue ice showing on north side of Western Cwm (WC), Lhotse face too shadowed to see well, but some blue ice evident.
The snow line on Mount Everest Region glaciers on Nov. 15, 2023 indicated by yellow dots on the Landsat image. Note that Nangpa La and Nup La-two high passes are both snow covered. The average snow line is 5800 m.
The snow line on Mount Everest Region glaciers on Oct. 30, 2023 indicated by yellow dots on the Landsat image. Note that Nangpa La and Nup La-two high passes are both snow covered. The average snow line is 5700 m.
Khumbu Glacier Icefall velocity from NASA ITS LIVE. Green arrows indicate primary range
Everest Base Camp Precipitation from the National Geographic Perpetual Planet station.

Great Glacier Retreat 1965-2023 Leads to formation of “Great Lake”

On By mspeltoIn Glacier Observations
Great Glacier terminus change from 1986-2022 illustrating lake expansion. Red arrow=1986 terminus location, Yellow arrow=2022 terminus location. Terminus has retreated 2.1 km during this time with the lake growing 15 km2.

Great Glacier is the largest outlet glacier of the Stikine Icefield feeding the Stikine River. The name came from the large expanse of the glacier in the lowlands of the Stikine River during the late 19th and early 20th century, that has now become a large lake. In 2023 I worked on a signage project for the Great Glacier Provincial Park with Hailey Smith, BC Park Ranger, documenting the changes in this glacier particularly since 1914.

The glacier filled what is now a large lake at the terminus of the glacier pushing the Stikine River to the east side of the valley. The Tahltan nation oral history relates when the glacier bridged the Stikine River and meet Choquette Glacier. In 1914 the glacier was easy to ascend from the banks of the Stikine River, the picture above is from the National Railroad Archive. By 1965 the new lake had formed, but the glacier still reached the far side of the lake in several places as indicated by the 1965 Canadian Topographic Map below. R. Patterson (Writer and Canadian Explorer 1898-1984) noted that Great Glacier came down onto the river flats, and displayed a 7 km front visible from the Stikine River.

Map of Great Glacier in 1965 illustrating the fringing lake.
Landsat images from 1990 and 2022, illustrating changes in the glacier and lake. The transient snowline is at ~900 m in both images.

A comparison of 1986, 1990, 2011 and 2022 illustrates the retreat. By 1986 the new lake had largely developed, and the glacier was beginning to retreat into the mountain valley above the lake. Retreat from the moraines of the late 19th century was 3200 m. By 2011 the glacier had retreated further into valley, 900 m retreat from 1986-2011. From 2011 to 2022 the glacier retreated another 1200 m. The lake has expanded to an area of 15 km2

A view of the glacier from across the lake today indicates the distance to the now valley confined glacier, and the trimlines of the former ice surface, yellow arrows in middle image The Great Glacier has one major tributary on the northeast tributary that is very low in elevation with a top elevation of 800 m. Given the regional snowline of 1100-1200 meters in the 1980s (Pelto, 1987) this is too low to retain snowcover through the summer and will lead to rapid progressive thinning. In 2018 and 2019 the highest observed snowlines in the region occurred, the snowline averaged 1500 m, leaving just 10% of the Great Glacier snowcovered. This is instead of the 60% needed to maintain equilibrium. Stikine Icefield outlet glaciers are all undergoing substantial retreats including Sawyer Glacier, Baird Glacier and Dawes Glacier.

Great Glacier snowline end of summer in 2018 and 2019 reached the highest levels observed at 1500-1600 m.