News

Roundup: Avalanches, Droughts, and a Sherpa protest

Posted by on Jun 5, 2017 in All Posts, Featured Posts, News, Roundup, Science | 0 comments

Roundup: Avalanches, Droughts, and a Sherpa protest

Spread the News:ShareRoundup: Avalanches, Droughts, and Sherpas   Calving Event in Peruvian Lake Damages Infrastructure Designed to Reduce Flood Risk From El Comercio: “Small ice avalanches have damaged the system of syphons in Lake Palcacocha, Ancash, Peru. Marco Zapata, the head of the Glacier Research Unit at INAIGEM, stated that on May 31, around 8 p.m., a calving event occurred at the glacier front on Mount Pucaranra, releasing ice into the lake. This event generated waves 3 meters in height, which caused 10 of the syphons to shift and which destroyed three gauges and a water level sensor.” Find out more about Lake Palcacocha and ice avalanches here.   Asian Glaciers Fight Against Drought From Nature: “The high mountains of Asia… have the highest concentration of glaciers globally, and 800 million people depend in part on meltwater from them. Water stress makes this region vulnerable economically and socially to drought, but glaciers are a uniquely drought-resilient source of water. Glaciers provide summer meltwater to rivers and aquifers that is sufficient for the basic needs of 136 million people… Predicted glacier loss would add considerably to drought-related water stress. Such additional water stress increases the risk of social instability, conflict and sudden, uncontrolled population migrations triggered by water scarcity, which is already associated with the large and rapidly growing populations and hydro-economies of these basins.” Find out more about Asia’s drought-resilient glaciers here.   Sherpas Demand Summit Certificates at Protest From The Himalayan Times: “Hundreds of sherpa climbers who met at Mt Everest base camp [in May] asked the government to immediately issue their summit certificates… Sherpa climbers who made it to the top of several peaks, including Mt Everest, have not been getting their summit certificates since last year after the government refused to approve their ascents citing a clause of the Mountaineering Expedition Regulation that bars them from obtaining such certificates… For most of the foreign climbers, summiting a mountain without sherpas’ help is almost impossible in Nepal… The new amendment to the regulation will recognize high-altitude workers as a part of the expedition to get certificates.” Find out more about the Sherpa protest and resolution here.     Spread the...

Read More

Cracks in the Paris Agreement

Posted by on Jun 1, 2017 in Editorial, Featured Posts, News, Uncategorized | 0 comments

Cracks in the Paris Agreement

Spread the News:ShareMajor cracks have appeared in recent months in Petermann Glacier in Greenland and the Larsen C Ice Shelf in Antarctica. These cracks are advancing and will soon release enormous icebergs into the ocean, one the size of the state of Delaware. They will allow ice from the interior of Greenland and Antarctica to flow into the ocean, contributing to sea level rise. Coastal areas in the U.S. will experience increased flooding, disrupting ports and airports, and interfering with the American economy that Trump claims to support, as well as causing harm to societies and ecosystems around the world.   And today a major crack appeared in the Paris Agreement, with Trump’s announcement of his intention to pull the U.S. out of it. This crack threatens to release, not icebergs, but distrust and despair, and disrupt the mechanisms that had begun to slow down global greenhouse gas emissions. This crack— in policy agreements rather than in masses of ice— can be sealed, by efforts of other countries, and of states and cities in the United States and by actions of the corporations and organizations that sought to keep the U.S. in the agreement.   The laws of physics indicate that ice will continue to flow from Greenland and Antarctica, at least as long as global warming is not abated. But the processes within global society are not as inevitable. With concerted action, the Paris Agreement can still be a vital force to preserve our planet from one of the greatest threats it has ever faced. Spread the...

Read More

Learning from a Flood-Alarm System’s Fate

Posted by on May 31, 2017 in Adaptation, All Posts, Featured Posts, News, Policy and Economics | 0 comments

Learning from a Flood-Alarm System’s Fate

Spread the News:ShareA longer version of this post appeared in the April 2017 issue of EcoAmericas. When a flood from a mountain lake threatened to swamp the town of Carhuaz in the Peruvian Andes early one morning in April 2010, Víctor Rodríguez was the only person who knew. From his hut on a plain below the mountain, he heard the jet-like rumble as a block of ice calved off a glacier and crashed into the lake. The force of the fall produced a wave that swept over the earthen dike around the water body, called Lake 513, and cascaded down the steep slope. Rodríguez watched as the water swirled across the plain, swamping the catchment for the municipal water system, where he worked as caretaker. Picking up speed as it funneled into the Chucchún River, the torrent of water carrying mud and boulders swept away crops, livestock and some buildings. But it stopped just short of the town of about 12,000 people beside the Santa River, at the foot of Peru’s Cordillera Blanca. The Destruction of an Early-Warning System With climate change increasing the threat of such hazards, the Swiss government’s development agency, a Peruvian nonprofit, and a Swiss university teamed up to develop a high-tech early-warning system. By the end of 2013, lakeside sensors and cameras were in place above Carhuaz, with relay antennae that could transmit information quickly to a command center in the municipal offices. Once its kinks were worked out, the organizers of the project hoped the system could serve as a model for other towns that lie below glacial lakes. Then disaster struck again, this time in the form of a drought. Not only was rain scarce, but an unseasonable frost damaged crops. Rumors spread among residents of the farming communities around Carhuaz that the monitoring equipment at Lake 513 was preventing clouds from forming. Early one morning last November, several hundred people from the largely indigenous communities, where traditional Andean beliefs still hold sway, trekked up to the lake and tore down the system. Within a week, it rained. The events raise questions about how to ensure that in areas where rural residents distrust technology, systems can be created to reliably warn those in the path of Carhuaz-style deluges, known as glacial lake outburst floods, or GLOFs. It also highlights tensions between growing urban areas and their rural neighbors— tensions that could deepen as dense development encroaches on agricultural land and city dwellers demand a larger share of water from threatened sources. The destruction of the Carhuaz early-warning equipment came as a shock to the system’s developers, but in hindsight, signs of discontent had been building. During workshops in 2012, residents said they felt unprotected against outburst floods like the one in 2010, says Karen Price Ríos of CARE Peru, a nonprofit development organization that has been active in the area for several years. Price worked with local communities on the three-year early warning project, which was funded by the Swiss aid agency COSUDE and supported by researchers from the University of Zurich. The researchers drew up a risk map, showing the areas in varying degrees of danger from a mudslide like that of 2010, and devised evacuation routes, marking them with signs. The centerpiece of the project was the early-warning system on Mount Hualcán. If a block of ice broke from the glacier and crashed into Lake 513, it would trigger sensors that would turn on cameras and send an alert to local officials. They could then check the images from the cameras to verify the flood and sound an alarm. The...

Read More

Let it Snow… and Save a Glacier

Posted by on May 30, 2017 in All Posts, Featured Posts, News | 0 comments

Let it Snow… and Save a Glacier

Spread the News:ShareNews about shrinking glaciers is not uncommon, but have you ever heard of regrowing one artificially? That is exactly what a team of researchers intends to do: use snow machines, also known as Schneekanonen (snow-cannons) in German, to save Morteratsch Glacier in the Swiss Alps. Felix Keller, a glaciologist at the Academia Engiadina in Switzerland, and Johannes Oerlemans, director of the Institute for Marine and Atmospheric Research at Utrecht University in the Netherlands, will use snow machines to slow down, or even reverse, the retreat of the glacier as announced at the annual meeting of the European Geosciences Union in Vienna, Austria, on April 27th. Morteratsch, located in Pontresina in the canton of Graubünden, is the third largest glacier in the Eastern Alps. It is also one of the most easily accessible glaciers: a 50-minute walk from Morteratsch train station along a hiking trail leads visitors directly to the glacier tongue. This makes it a popular tourist attraction that contributes to the economy of the region. However, the glacier has been shrinking rapidly because of climate change, retreating about 2.5 kilometers over the last 150 years. The plan to save the glacier using snow machines was inspired by the successful use of white fleece coverings to slow down the retreat of the nearby Diavolezzafirn Glacier. This method has been applied over the past 10 years to help the glacier grow by up to 8 meters in length. Locals reached out to Oerlemans and Keller, who have done prior research in the region, to try to save Morteratsch in a similar manner, except the latest plan involves covering sections of the glacier with snow to reduce melting during the summer. “The municipality of Pontresina, in whose territory the glacier is situated, is trying to position itself as a village at the forefront of climate change issues,” Daniel Farinotti, a glaciologist at both Swiss Federal Institute of Technology (ETH) in Zurich and the Swiss Federal Institute for Forest, Snow and Landscape Research (WSL), shared in an interview with GlacierHub. A layer of snow will protect the ice from incoming radiation, which would warm up the glacier. A secondary and smaller effect would be to protect the ice from overlying air, which could be above freezing. Models used by the researchers suggest that a thin layer of snow covering under one square kilometer at the top of the glacier would be enough to protect the glacier. Oerlemans also estimates that this could help the glacier regain 800 meters of length in two decades. This plan would involve the use of 4,000 snow machines, which produce snow from water and pressurized air. They will be supplied with meltwater from a nearby glacier, which addresses a key concern: “If we want to do it on a larger scale, the main challenge will be the availability and transportation of meltwater onto the glacier,” Oerlemans shared with GlacierHub. Not everyone is convinced that the plan will work. “I am still a little skeptical that the technical problems are solved and would like to see answers to some questions,” Greg Greenwood, executive director of the Mountain Research Initiative, shared with GlacierHub. These questions include exactly where the snow will be deposited, financial and environmental costs, and a comparison with other technical options. Oerlemans and Keller are currently conducting a pilot project costing $100,000 at the foot of Diavolezzafirn glacier, also in Switzerland. 13 feet of snow will be blown over the 1,300-square-foot glacier by the end of the month. If it works, they hope that the Swiss government will fund the Morteratsch project, which will cost several million Swiss...

Read More

No-Fly Zone Administered Over Glacier Crash Site

Posted by on May 24, 2017 in All Posts, Featured Posts, News | 0 comments

No-Fly Zone Administered Over Glacier Crash Site

Spread the News:ShareIn 1952, a military plane crashed into Mount Gannett, 50 miles east of Anchorage, killing all 52 service members on board. The plane was located in 2012 at Colony Glacier, but it has taken years to retrieve the remains as rescuers can only travel to the crash site in June, when conditions are safest on the glacier. Over this time, the receding glacier has made the crash site more visible, but it has also enticed sightseers on helicopters, who risk disturbing the remains or removing artifacts. As a result, a no-fly zone has been administered this month by the Federal Aviation Administration to stop people from disturbing the crash site. To date, 35 human remains have been repatriated, but it may take several more years to retrieve the remaining 17. The plane went down in the Chugach Mountain range, one of the snowiest locations in Alaska. During the winter of 1952-1953, in the Chugach’s Thompson Pass, a record 81 feet of snow was recorded. Colony Glacier remains dangerous due to deep crevasses, variable weather and sharp pieces of ice. Douglas C-124 Globemaster II, "Old Shaky," was built in Long Beach, CA. Could carry 68,500 lb of cargo. #avgeek #lift pic.twitter.com/WURPDu4NvL — SDASM L&A (@SDASM_archives) September 4, 2014 Erin Pettit, an associate professor of glaciology at the University of Alaska at Fairbanks, told GlacierHub about similar plane crashes that have been buried beneath glaciers. “There are a handful around the world – at least one in Greenland and one in Antarctica. Sometimes they weren’t ‘lost’ in the sense that no one knew what happened, but they just couldn’t extract the plane,” she said. “The plane was absorbed by the glacier and won’t re-emerge for hundreds or even thousands of years, depending on where it landed and how big the glacier is.” When a plane crashes into a glacier, it is covered by snowfall and over time freezes into the glacier. When the glacier moves downslope, the plane moves along with it, until it is later revealed at the front of the glacier. Warmer temperatures speed this process up. Bob McNabb, a glaciologist at the University of Alaska, calculated the speed and trajectory of the flowpath of the Colony Glacier and made a map for GlacierHub. Using a back-of-the-envelope calculation, McNabb said the plane traveled 23 kilometers along the flowpath, which means it would have traveled one meter per year. Using this analysis, which involved the use of satellites, McNabb calculated that the average surface velocity would have been about 1.5 meters per year. Michael Loso, a physical scientist at Wrangell-St. Elias National Park and Preserve, told GlacierHub that Colony Glacier has a velocity of about 3 feet per day, saying, “That’s fast but not unreasonably fast for a big Alaskan glacier.” Alaska has a higher rate of plane crashes than the rest of the United States for reasons like frequent inclement weather, jagged terrain, which can be obscured by clouds, and the fact that flying is the only way to get to certain remote places. The cause of the 1952 crash has never been determined. Loso added that such crashes at glaciers are not that uncommon, saying, “Many glaciers are in mountains, and planes run into mountains every once in awhile.” Colony Glacier Chugach State Park Alaska pic.twitter.com/9FRYV8svnH — Mark Stadsklev (@artwithinnature) April 18, 2017 Spread the...

Read More

Don’t Step on the Crack at Petermann Glacier

Posted by on May 18, 2017 in All Posts, Featured Posts, News, Science | 0 comments

Don’t Step on the Crack at Petermann Glacier

Spread the News:ShareCracks in ice shelves have appeared in disaster movies as ominous signs of global warming. One memorable instance occurs in The Day After Tomorrow when a paleoclimatologist is drilling ice cores at the Larsen Ice Shelf. The shelf breaks apart, leading to a series of cataclysmic climate events that disrupt the North Atlantic Ocean circulation. In July, a real- life crack appeared at Petermann Glacier in Greenland and has been growing steadily ever since. Two scientists, Andreas Muenchow and Keith Nicholls, are investigating the crack and hypothesize that it is caused by an increase in air and ocean temperatures. Petermann Glacier connects the Greenland ice sheet to the Arctic Ocean at 81°N. It is approximately 43 miles long and nearly 10 miles wide. This is not the first crack or full break of ice at Petermann Glacier, according to a Washington Post article by Chris Mooney. Since 2010, entire slabs of the Petermann glacier have broken off. In fact, during two occasions, the glacier lost an area of ice six times the size of Manhattan, according to Mooney. This loss raises enormous concern because the glacier serves to slow down the flow of ice downhill from the Greenland ice sheet into the ocean. For this reason, experts call Petermann a “floodgate.” If the glacier that sits behind Petermann melts, it could raise sea levels by about a foot. A recent paper published in the Geophysical Research Letters describes this type of calving at Petermann as common. The authors explain that it is usually assumed that ocean-ice dynamics are not involved. However, evidence from the Pine Island Glacier in West Antarctica found that ocean forcing can play a role in the melting. Muenchow and Nicholls expect similar dynamics are occurring with Petermann Glacier. They have been on several expeditions to the glacier in order to measure ocean temperatures underneath the shelf itself. They want to see if rising ocean temperatures are also detrimental to the glacier and causing the melting from below. If warm ocean water were melting the base of the glacier, it would only accelerate the destruction of Petermann. While it is extremely difficult to know definitively, they hypothesize Petermann’s river and the channel beneath it are playing a role in the melting. Data from 2015 and 2016 demonstrates that the temperatures of the warm Atlantic layer in the ocean have increased. With both air and ocean temperatures getting warmer, it is unclear how much longer Petermann Glacier will be intact, leaving frightening implications for the melting of the enormous glacier behind it. The crack in the Petermann Glacier and the possible ensuing events show that news from the ice can sometimes be just as scary as the scenes in disaster movies. Spread the...

Read More