Large Hydropower and Water-storage Potential in Future Glacier-free Basins
A major study published in Nature takes a global look at the hydropower potential of deglacierized water basins. As glaciers retreat in high mountain areas, they sometimes expose areas which can be used as hydropower reservoirs by holding snowmelt and runoff from rain. From the abstract:
“Climate change is causing widespread glacier retreat, and much attention is devoted to negative impacts such as diminishing water resources, shifts in runoff seasonality, and increases in cryosphere-related hazards. Here we focus on a different aspect, and explore the water-storage and hydropower potential of areas that are expected to become ice-free during the course of this century…Although local impacts would need to be assessed on a case-by-case basis, the results indicate that deglacierizing basins could make important contributions to national energy supplies in several countries, particularly in High Mountain Asia.”
A Glacial Erratic is the Star of a New Children’s Book
A children’s book entitled Old Rock (Is Not Boring), written an illustrated by Deb Pilutti, features rocks and glaciers. From a review of Old Rock (Is Not Boring):
“Old Rock sits “in the same spot, at the edge of a clearing in the middle of a pine forest” every day, and the other forest residents insist the rock must be bored. After Hummingbird, Spotted Beetle, and Tall Pine regale Old Rock with tales of their adventures, Old Rock relays a rich history in which he was shot from a volcano, hid dinosaurs from predators, survived an ice age, traveled frozen in a glacier, and rolled onto plains populated with mastodons.”
Kyrgyz Herders Follow Glacial Melt, Study Finds
Kyrgyz herders in Central Asia use proximity to glaciers as a criteria for selecting which kinds of pasture are best for their flocks, according to a recent study in the journal Ecology and Society. From the abstract:
“Consensus on the state of rangelands is often elusive. This is especially true in the primarily agropastoral former Soviet republic of Kyrgyzstan. Some argue Kyrgyz rangeland is being rapidly degraded by overgrazing. However, poor data and climatic changes confound this assessment. Thus there is contention amongst researchers, state officials, and local agropastoralists about the etiology and appropriate degree of concern regarding changes in flora and landscape patterns. This lack of consensus makes pasture management difficult for local elected managers. In this study, we use audiovisual primes, structured interview tasks, and consensus analysis to examine the degree of agreement among local agropastoralists of Naryn oblast about (a) the nature of several degradation-ambiguous plant and landscape types found in the area, and (b) indicators of “good” pasture. We find relatively little interparticipant agreement on high-resolution details, but a pattern of consensus regarding (i) a refutation of select species as indicators of degradation, as well as (ii) apparent shared heuristics for determining what makes for good, versus bad, pasture. We consider socio-historical and cognitive drivers of these patterns, and close with a discussion of implications for management.
Global warming will cause substantial glacier retreat for the majority of the world’s glaciers over the next few decades. This will not only spell the end for some magnificent natural monuments, but also importantly affect the water cycle. In high-mountain regions, these ice masses act as reservoirs feeding water to large river systems, and balancing seasonal discharges.
Without glaciers, rivers would carry considerably less water in summer, which would have noticeable consequences for water availability, energy production and agriculture in many regions of the world. Researchers had previously discussed the idea of compensating the shrinking storage function of glaciers with reservoirs (see Zukunftsblog – in German only).
A group of glaciologists from ETH Zurich and the Swiss Federal Institute for Forest, Snow and Landscape Research WSL is now again engaging in the discussion about the dwindling ice: in a study published in Nature, they investigate the global potential for storing water and producing hydropower in presently-glacierised areas that will become ice-free within this century.
Using glaciers as reservoirs
In their study, the research team around Daniel Farinotti, Professor of Glaciology at the Laboratory of Hydraulics, Hydrology and Glaciology (VAW) at ETH Zurich and at WSL, analysed about 185,000 glaciers. For these sites they calculated a maximum theoretical storage potential of 875 cubic kilometers (km3) and a maximum theoretical hydropower potential of 1350 terawatt hours (TWh) per year.
“This theoretical total potential corresponds to about one third of current hydropower production worldwide. But in reality, only part of it would be realisable”, explains Farinotti.
In order to obtain a more realistic estimate, the researchers conducted an initial suitability assessment for all sites. They identified around 40 percent of the theoretical total potential as “potentially” suitable, equalling to a storage volume of 355 km3 and a hydropower potential of 533 TWh per year. The latter corresponds to around 13 percent of the current hydropower production worldwide, or nine times Switzerland’s annual electricity demand.
“Even this potentially suitable storage volume would be sufficient to store about half of the annual runoff from the studied glacierised basins,” Farinotti says. Assuming an average climate scenario, about three-quarters of the storage potential could become ice-free by 2050.
Cautious estimate of potential
For their analysis, the glaciologists used a global glacier inventory and placed virtual dams at the current terminus of each glacier with an area of more than 50,000 square meters located outside the Subantarctic. They then optimised the size of the reservoirs by appropriate dam positioning and height. In doing so, they minimised the reservoirs’ impact on the landscape and did not just maximise economic return. The team used digital elevation models of the subglacial terrain and combined them with a glacier evolution model to determine the storage volume of the 185,000 glaciers they had selected.
In the suitability analysis that followed, the researchers assessed the sites based on several ecological, technical and economic criteria: “On this basis, we ruled out the most unsuitable sites; this enabled a more realistic assessment,” explains co-author Vanessa Round, who was affiliated at both institutions and had a pivotal role in the study. She also adds that it is neither realistic nor desirable to build a dam for every glacier.
A model for the future?
The team also stresses that local impacts should be assessed on a case-by-case basis. Nevertheless, the results indicate that deglacierised basins could significantly contribute to national energy supply and water storage in a number of countries, particularly in High Mountain Asia.
Among the countries with the largest potentials are Tajikistan, where the calculated hydropower potential could account for up to 80 percent of current electricity consumption, Chile (40 percent) and Pakistan (35 percent). In Canada, Iceland, Bolivia and Norway, the potential equals 10–25 percent of their current electricity consumption. For Switzerland, the study shows a potential of 10 percent.
Meanwhile, the Swiss Federal Office of Energy has recently revised downwards the expansion potential for Swiss hydropower. This is mainly because of revised estimates for the impact of stricter regulations on environmental flows, and because the potential of small-scale hydropower is now considered to be lower than it was in 2012. However, in its assessment, the SFOE explicitly excluded the hydropower potential that could arise from future ice-free basins. For this reason, the glaciologists led by Farinotti do not see a contradiction to their results, as the two studies cannot be directly compared.
This post was written by Michael Keller and originally published by ETH Zurich.
A case study of the impact of climate change on alpine hydropower
From the journal Water: “Greenhouse gas reduction policies will have to rely as much as possible upon renewable, clean energy sources. Hydropower is a very good candidate, since it is the only renewable energy source whose production can be adapted to demand, and still has a large exploitation margin, especially in developing countries. However, in Europe the contribution of hydropower from the cold water in the mountain areas is at stake under rapid cryospheric down wasting under global warming. Italian Alps are no exception, with a large share of hydropower depending upon cryospheric water. We study here climate change impact on the iconic Sabbione (Hosandorn) glacier, in the Piemonte region of Italy, and the homonymous reservoir, which collects water from ice melt.”
Water availability in Pakistan under Paris Agreement targets
From the journal Advances in Water Resources: “Highly seasonal water supplies from the Himalayan watersheds of Jhelum, Kabul and upper Indus basin (UIB) are critical for managing the world’s largest contiguous irrigation system of the Indus basin and its dependent agrarian economy of Pakistan. Here, we assess changes in the contrasting hydrological regimes of these Himalayan watersheds, and subsequent water availability under the Paris Agreement 2015 targets that aim of limiting the mean global warming to 1.5 °C (Plus1.5), and further, well below 2.0 °C (Plus2.0) relative to pre-industrial level.”
Measuring ambient black carbon near India’s Gangotri Glacier
From the journal Atmospheric Environment: “The warming effect of equivalent Black Carbon (EBC) aerosols due to their light absorbing nature is a serious environmental concern, particularly, in the eco-sensitive and glaciated Himalayan region. Moreover, baseline data on BC is rarely available from most of the glaciated Himalayan region. For the first time, measurements on ambient EBC mass concentration were made at a high altitude site Chirbasa (3600 m, amsl), near Gangotri Glacier in the Indian Himalaya, during the year 2016. The change in the EBC concentration over the year was recorded from 0.01 μg m−3 to 4.62 μg m−3 with a diurnal variability of 0.10 μg m−3 to 1.8 μg m−3. The monthly mean concentration of EBC was found to be minimum (0.089 ± 0.052 μg m−3) in August and maximum (0.840 ± 0.743 μg m−3) in the month of May. The observed seasonal mean concentrations of EBC are less than 0.566 μg m−3 whereas the annual mean is 0.395 ± 0.408 μgm−3 indicating a pristine glacial and absence of locality EBC sources. Further, investigation on the occasional high values extricated that the seasonal cycle of EBC was significantly influenced by the emissions resulting from agriculture burning (in western part of the country), forest fires (along the Himalayan slopes) in summer, and to some extent the contribution from long range transport of pollutants in winter, depending the prevailing meteorological condition.
For many people, climate change feels like a distant threat—something that happens far away, or far off in the future. Scientists and climate communicators often think that if everyone saw the devastating impacts of climate change, we’d all be more likely to accept it as real, and that accepting climate science is essential to taking action against it. A new study, published this month in Regional Environmental Change, challenges the latter part of this assumption.
The study examined decision-making in three places affected by melting glaciers. For these communities in the Italian Alps, the Peruvian Andes, and the US’s North Cascades, glacier retreat is a visible fact—“and the causes of glacier retreat are almost exclusively warming,” explains lead author Ben Orlove, an anthropologist and co-director of the Center for Research on Environmental Decisions at Columbia University’s Earth Institute. (Orlove is also the managing editor of GlacierHub.)
Orlove and his colleagues wondered whether the people who live in the three locales notice these changes, whether they understand them to be the result of climate change, and whether this climate connection motivates them to take action.
They found that people in these villages are indeed aware of climate change and are even taking action to adapt to it. But the villagers don’t often talk about climate change as a motivation for adapting. Instead, they’re more likely to look closer to home for reasons to respond to the changing environment, focusing on how the responses can benefit their communities. The study suggests one potential way to reframe the conversation around climate adaptation and make it more appealing.
Exploring different frames of mind
Orlove’s team looked at the frames of thinking that mountain-dwellers use to understand the changes happening around them. Mental “frames” help us sort new information and reconcile it with our previous knowledge and beliefs. For example, says Orlove, “If a hydropower plant in the Italian Alps doesn’t get enough water to generate electricity, what kinds of associations do the villagers make when they think or talk about these changes?”
The team examined how mountain-dwellers utilized two frames when talking about glacial retreat. The first was a climate change frame that focuses on global changes and the need for global solutions. The second was a community frame emphasizing action at a local level and recognizing positive opportunities for local advancement, in addition to the negative challenges of environmental change.
By analyzing peoples’ speech patterns during in-depth interviews, focus groups, and in records of community meetings, the researchers investigated how often people in the mountain communities used these two frames when talking about the impacts of climate change.
Different regions, different challenges, similar framing
The study found that villages in all three research sites are undertaking actions that could be described as adaptations to climate change. However, the communities themselves don’t always think of their actions that way. The authors present three cast studies.
Tourism in the North Cascades
Glaciers, rivers, lakes, and snowpack draw tourists to the slopes of Mount Baker in Washington State, providing the major source of income for the towns of Concrete and Glacier. But those natural resources are at risk as the planet’s temperature climbs.
Orlove’s team argues that these communities in the North Cascades are adapting to glacial retreat by finding ways to expand other forms of tourism. One example is through festivals that celebrate historical heritage and wildlife, and help to bring the community together.
A firemen’s muster during the Cascade Days festival in Concrete, Washington. The study authors argue that festivals like this help to attract tourism independent of the area’s disappearing glaciers, and thus could be considered an adaptation to climate change. (Source: Ben Orlove)
However, Concrete and Glacier residents rarely used words associated with the climate change frame when describing the changes or the local response. Instead, they use a community frame, emphasizing the importance of bolstering tourism and supporting livelihoods and the next generation.
“These kids who get out of high school, there’s not much for them to do except go out of town and find a job in [the nearby town of] Mount Vernon or Seattle,” said one interviewee. “Some of them of course go to college, but probably the majority of them don’t. So there’s no real way to make a livelihood up here. We’re dependent on tourism.”
Hydropower in the Italian Alps
As glaciers in the Italian Alps shrink, river levels are declining, reducing the ability of hydropower plants to generate electricity. To keep up with demand, the villages of Trafoi, Stilfs, and Sulden have installed biomass generators that burn wood chips to generate electricity, and the extra heat gets piped into homes.
The researchers found that although residents sometimes describe the wood chips as a renewable resource — a term from the climate change frame — they’re more often to rely on the community frame. Many villagers mentioned liking the wood heat for its coziness, and emphasized that that the wood chips are a local resource that supports local independence. Others mentioned the next generation, noting that the wood chip industry provides local jobs and that the pipes have provided conduits to install fiber optic cables; both of these encourage younger people to stay in their communities rather than seeking a future elsewhere.
Water in the Peruvian Andes
The village of Copa in the Peruvian Andes is also watching its water supply fall. Meanwhile, its need for water has only increased, as warmer temperatures and irregular rainfall make crop irrigation more important.
To adapt to these changes, Copa has upgraded its water infrastructure to reduce water leakage. It is using concrete to line the canals that carry water from the river, and building pipe systems to bring water into homes instead of hauling buckets from the canal. As with the previous examples, these developments are most often seen through a community frame, with a focus on how the modern water system earns recognition for the village. “They speak with pride of the village square,” says Orlove, “with piped water giving it a more urban look.”
By the numbers
Using both human judgment and computer keyword analysis, Orlove and his team analyzed how often people in these communities referred to environmental changes, whether they attributed these changes to climate change, and whether they described their activities as adaptive responses to the ongoing changes.
They found that the villagers frequently talk about climate change impacts. In interviews, focus groups, and community meetings, changes in ice, water, socioeconomic changes, weather, and agriculture come up in about 13 percent of conversation turns (defined as the words that one person speaks without interruption). “In other words,” the paper notes, “they do not find climate change hard to see.”
However, people linked these alterations to climate change in only 4 percent of the conversation turns, and they describe their actions as adaptive responses in only 5 percent of conversation turns. Overall, people were five times more likely to refer to the community frame than the climate change frame (4.83 percent versus 0.93 percent).
Reframing the conversation
In each of the case studies, communities see the effects of climate change and take steps to address the impacts. Yet they do all of this without making much use of climate change terminology. While the villagers believe in climate change and do occasionally bring it up in conversation, the community is more relevant for them.
To Orlove and his colleagues, this challenges the notion that people need to ‘believe’ in climate change in order to take action against it. Furthermore, the authors write, “it could be argued that the community frame is more effective than the climate change frame because it emphasizes ‘co-benefits’ of adaptation” — such as protecting local resources from outsiders, retaining control over energy production, and increasing one’s connection to their community.
The findings emphasize that climate change communication should be more of a dialogue than a one-way conversation, and that scientists can learn a great deal from the communities they work with.
“It’s not that the only solutions are found in these locally organized communities,” says Orlove, “but people have not often looked for resources there, and when you do, you’ll see that there is social capital. People value their town, and they know each other and interact. They care about their environments and about their communities. We can recognize that as a resource that shouldn’t be overlooked at a time when climate needs far exceed available funds.”
This ability of people to engage with their neighbors and to craft solutions they care about could be helpful outside of mountain villages as well, says Orlove. “If we see self-organizing here, can we see self-organizing in other places, like in New York?”
This article originally appeared on State of the Planet, a news site for Columbia University’s Earth Institute.
From American Geophysical Union: “To this day, the ice volume stored in the many glaciers on Svalbard is not well known… This surprises because of the long research activity in this area. A large record of more than 1 million thickness measurements exists, making Svalbard an ideal study area for the application of a state‐of‐the‐art mapping approach for glacier ice thickness….we provide the first well‐informed estimate of the ice front thickness of all marine‐terminating glaciers that loose icebergs to the ocean.”
Read more about scientific advancements in measuring glacier thickness here.
Hydropower in Iceland: Opinions of Visitors and Operators
From Journal of Outdoor Recreation and Tourism: “The majority of visitors are against the development of hydropower in Skagafjarðardalir. They believe that the associated infrastructure would reduce the quality of their experience in the region that they value for perceived notions of it being untouched and undeveloped. If the quality of their experience is reduced, so would their satisfaction with that experience.”
Read more about the views regarding the impact of a proposed hydroelectric plant on the tourist experience in Skagafjarðardalir here.
8 Experts Explain What Mountain Communities Need Most
“What happens [in the Third Pole] can affect over 1.4 billion people and have regional and global ramifications.” – Tandong Yao
“Researchers and the media tend to focus on big glaciers, but it’s the much smaller and much less glamorous glaciers and ice fields that are going to affect mountain communities the most.” – Anil Kulkarni
Read more about future difficulties mountain communities will face, and how they should be addressed here.
A recent study on the Borgne d’Arolla, a glacier-fed stream in the Swiss Alps, shows that there is less biodiversity among macroinvertebrates than expected in the summer and higher biodiversity than expected in the winter. Chrystelle Gabbud, a geologist at the University of Lausanne in Switzerland, and her associates, found that the rates of streambed disturbance in the Borgne d’Arolla were also much more frequent than normal observations of disturbance in glacial rivers, even during times of peak discharge. The team’s results were published in September in Science of the Total Environment and attribute the above biodiversity inversion phenomenon to the increased frequency of flushing events.
Why is it that glacier-fed rivers in the Alps are experiencing even more flushing events? Evidence points toward the impacts of global climate change, as rising temperatures influence increased glacial melting and sediment production during the summer months, which in turn means that flushing must be facilitated more often.
Summertime runoff in glacier-fed Alpine rivers is exceptionally useful for supplying water for hydroelectric power production. The flow of water is abstracted at water intakes, which hold back both water and sediment, functioning similarly to dams but on a smaller scale. Intakes also have a relatively low threshold for how much sediment can accumulate before they must be flushed. This means that in basins with high erosion, namely glaciated basins, this flushing happens more frequently. In the summer months, when glacial melt is at its peak, flushing of water intakes can occur up to several times a day. Flushing disrupts the streambed, increases water turbidity, contributes to river aggradation, and negatively affects the macroinvertebrate community both in abundance and biodiversity.
Gabbud and fellow researchers collected samples of macroinvertebrates (animals that do not have a backbone but that are large enough to be seen with the naked eye, such as crustaceans, worms and aquatic insects) at several locations over the course of two years (2016 and 2017) to determine the impacts of flushing water intakes on species biodiversity and abundance. The surrounding tributaries served as controls for the Borgne. The researchers’ findings effectively contradicted the normal expectations for seasonal biodiversity changes.
Normal biodiversity expectations anticipate that both species richness and abundance should be higher during the summer months, from June to September, which also correspond to the highest water temperatures. However, Gabbud and her team found that biodiversity of macroinvertebrate populations in the Borgne d’Arolla during winter months (and coldest water temperatures) was comparable to the expected levels for the surrounding tributaries during the spring and summer. The Borgne was found to be mostly devoid of life in the summer months, a result which the researchers primarily attribute to the high frequency of flushings.
The team also compared observations in 2016 to those in 2017. Variations in flushing frequency and duration between the two years led Gabbud and her associates to two determinations. One, that more flushing had a direct negative impact on the presence of macroinvertebrate biodiversity and abundance. Two, that flushings with shorter duration also correlated with higher rates of streambed disturbance.
In addition, they found that as the frequency of flushing decreased, macroinvertebrate populations started to return. Outside of the summer months, flushing happens much less frequently. In a four-day period between flushes, biodiversity was almost able to reach pre-disturbance levels.
The researchers’ observations led them to recommend that the frequency of flushing at the water intakes be decreased and the duration of flushing be increased. They stipulate that higher magnitude flushings, resulting from taking too much time between events, could also have negative impacts. Thus, this situation creates a tension between maintaining hydropower and maintaining biodiversity, a major policy issue.
Currently, Switzerland has a single set of regulations regarding mitigating impacts and restoring ecological areas being used for hydropower generation. There are provisions related to sediment management; however, guidance provided by the Swiss National Government does not mention water intakes by name, instead only addressing dams and maintaining sedimentconnection.
Seeing as water intakes govern over 50 percent “of hydropower impacted rivers by basin area” in the Swiss Alps, Gabbud and her team emphasize that future regulations must incorporate both sedimentmanagement and flow management.
Scientific Tensions Among Early Glacier Researchers
From Isis: “Historians of science have long recognized the field as a socially heterogeneous space wherein different groups jostle for access and to assert the priority of their activities… The essay analyzes a dispute between a mountaineer and a scientist-mountaineer that took place at this time, in which the scientist turned to mountaineering ethics to confront accusations of pseudoscience.”
Hydropower and Glacier Shrinkage in the Italian Alps
From Applied Energy: “We assess the impacts of nine climate-change scenarios on the hydrological regime and on hydropower production of forty-two glacierized basins across the Italian Alps, assumed exemplary of similar systems in other glacierized contexts.”
Read more about hydropower in the Italian Alps here.
Declining Glacier Cover Threatens Biodiversity
From Global Change Biology: “Climate change poses a considerable threat to the biodiversity of high altitude ecosystems worldwide, including cold‐water river systems that are responding rapidly to a shrinking cryosphere… Using new datasets from the European Alps, we show significant responses to declining glacier cover for diatoms, which play a critical functional role as freshwater primary producers.”
The Importance of Snow Sublimation on a Himalayan Glacier
From Frontiers in Earth Science: “Snow sublimation is a loss of water from the snowpack to the atmosphere. So far, snow sublimation has remained unquantified in the Himalaya, prohibiting a full understanding of the water balance and glacier mass balance. Hence, we measured surface latent heat fluxes with an eddy covariance system on Yala Glacier (5,350 m a.s.l) in the Nepalese Himalaya to quantify the role snow sublimation plays in the water and glacier mass budget. Observations reveal that cumulative sublimation is 32 mm for a 32-day period from October to November 2016, which is high compared to observations in other regions in the world.”
Hydropower Production in India under Climate Change
From Nature: “Hydropower is a valuable renewable energy resource in India, which can help in climate change mitigation and meet the increasing energy demands. However, the crucial role of climate change on hydropower production in India remains unexplored. Here using the observations and model simulations, we show that seven large hydropower projects experienced a significant (p-value < 0.05) warming and a decline in precipitation and streamflow during the observed period of 1951–2007.”
From Molecular Ecology: “Primary succession on bare ground surrounded by intact ecosystems is, during its first stages, characterized by predator‐dominated arthropod communities. However, little is known on what prey sustains these predators at the start of succession and which factors drive the structure of these food webs. As prey availability can be extremely patchy and episodic in pioneer stages, trophic networks might be highly variable. Moreover, the importance of allochthonous versus autochthonous food sources for these pioneer predators is mostly unknown. To answer these questions the gut content of 1832 arthropod predators… were screened molecularly to track intraguild and extraguild trophic interactions among all major prey groups occurring in these systems. ”
From Mid-Day.com: “A school teacher and mother of a soldier was so inspired by the sacrifices made by the country’s jawans, that she decided to make one of her own. Pune resident, Sumedha Chithade, 54, has sold her ancestral gold bangles to raise funds to build an oxygen plant for soldiers posted at Siachen Glacier.”
Controversial Hydropower Along a Trans-Himalayan River
From Water Policy: “Teesta is one such mighty trans-Himalayan river flowing through India and Bangladesh and is recognized as a basin where there is increasing tension between these two nations. Due to upstream interventions including barrage, dam and hydropower construction, the lower riparian region of Bangladesh faces acute water stresses, which hampers the agricultural, fisheries and livelihood activities of the river-dependent communities and impedes the economic prosperity of the greater North-west region. The study provides a robust outline of the transboundary nexus between India and Bangladesh, and identifies upstream intervention-induced economic loss and ecological deterioration in the lower Teesta basin.”
From PNAS: “Supraglacial ice cliffs exist on debris-covered glaciers worldwide, but despite their importance as melt hot spots, their life cycle is little understood. Early field observations had advanced a hypothesis of survival of north-facing and disappearance of south-facing cliffs, which is central for predicting the contribution of cliffs to total glacier mass losses.”
A recent study in Nature by Hamish Pritchard, a glaciologist at Cambridge University and researcher for the British Antarctic Survey, shows that the high mountains of Asia, including the Himalayas, the Hindu Kush, and Karakoram, are being greatly affected by global warming. In some areas of the Himalayan region, for example, temperatures have risen faster than the global average. From 1982 to 2006, the average annual mean temperature in the region increased by 1.5 °C, with an average increase of .06 °C per year, according to UNEP. Even though studies on the high mountains of Asia are incomplete, it is believed that the mountains will lose half of their ice in the next 30 years.
This glacial loss has consequences for Asia as the glaciers provide an important ecosystem service to 800 million people by acting as a regional buffer against drought and providing summer meltwater to rivers and aquifers. If the glaciers in the eastern and central Himalayas disappear by 2035, the ecosystem service protecting against drought would be lost. Despite the fact that glaciers can promote drought resiliency, the surrounding areas would be particularly vulnerable to water scarcity because the glaciers will not supply enough meltwater to maintain the rivers and streams at adequate levels.
Lack of water could lead to devastating food shortages and malnutrition, further impacting the economy and public health. Based on a projected estimate of glacier area in 2050, it is thought that declining water availability will eventually threaten some 70 million people with food insecurity. Droughts in the Himalayan region have already resulted in more than 6 million deaths over the past century. Glacier loss would only add to drought-related water stress in the region, impacting a surrounding 136 million people.
In an interview with GlacierHub, Pritchard explained, “Without these glaciers, particularly in the Indus and Aral, droughts would be substantially worse in summer than they are now, and that could be enough to drive conflict and migration, which becomes a regional and potentially global issue. It could result in social instability, conflict, and migrations of populations.”
According to Pritchard’s research, the high mountains of Asia supply 23 cubic kilometers of water downstream every summer. If the glaciers were to vanish, the amount of water during the summer would decrease by 38 percent in the upper Indus basin on average and up to 58 percent in drought conditions. The loss of summer meltwater would have its greatest effects on the municipal and industrial needs of Pakistan, Tajikistan, Turkmenistan, Uzbekistan and Kyrgyzstan, with water stress being classified as medium to extremely high. For example, the Indus River, which has one of the world’s largest irrigation networks, is Pakistan’s primary source of freshwater. About 90 percent of Pakistan’s agriculture depends on the river and much of the world’s cotton comes from the Indus River Valley. Additionally, decreased meltwater would further affect upstream countries such as Kyrgyzstan, Tajikistan and Nepal that rely on hydropower. The Toktogul hydropower plant and four smaller plants downstream produce almost 80 percentof Kyrgyzstan’s electricity.
Pritchard presents data that show how much the glacier meltwater contributes to different regions within Asia during drought. Some areas, such as the Aral Sea, rely exclusively on the glacier water during the drought months. The glaciers provide meltwater when rainfall is minimal or nonexistent under drought conditions because glaciers store precipitation for decades to centuries as ice, which then flows to lower altitudes when melting in the summer. Twila Moon, a postdoctoral research associate at the U.S. National Snow and Ice Data Centre in Boulder, Colorado, recently discussed the consequences of global glacier volume loss on populations worldwide in Science magazine. “Rising seas, to which melting ice is a key contributor, are expected to displace millions of people within the lifetime of many of today’s children,” she stated. “This loss of Earth’s land ice is of international concern.”
As temperatures continue to rise, the surrounding regions will begin to lose their source of water for food, agriculture and survival. Due to inadequate scientific studies and evidence, the trends and status of glaciers in the Himalayas and other ranges are not being sufficiently observed and recorded. A lack of adequate monitoring of the glaciers means political action to adapt to the foreseen changes will be limited. More communication between the scientific community and policymakers is needed to relay knowledge about the impacts of changes in glaciers on the region’s hydrology, environment and livelihoods.
Any Star Wars fan will recognize the remote ice planet Hoth, the location of some of the most iconic scenes from Episode V: The Empire Strikes Back, including the attack on the Rebel Alliance’s Echo Base by Imperial Walkers and Han Solo’s daring rescue of Luke Skywalker after his tauntaun was attacked by a wampa. Not many people, however, would know that those legendary scenes were filmed on a Norwegian ice cap called Hardangerjøkulen.
When the movie was filmed in 1980, the crew had to cope with subzero temperatures and freezing winds. However, nearly forty years later, the real-life Hoth is disappearing. According to a recent paper by Henning Akesson et al., published in The Cryosphere, the ice cap is extremely sensitive to small changes in temperature, and therefore vulnerable to climate change as global temperatures continue to increase.
Akesson explains in an article for ScienceDirect that due to increasing temperatures, it is feasible that Hardangerjøkulen could fully melt by 2100 if the trends continue. Once it melts, he and his team maintain that the ice cap will never return.
As the authors of the study explain, Hardangerjøkulen is located in southern Norway and measured 73 square kilometers as of 2012. It is generally flat in the interior and has several steeper glaciers along the edge of the ice cap that drain the plateau. Two of these glaciers, Midtdalsbreen and Rembesdalsskaka, have retreated 150 meters and 1386 meters respectively since 1982. Akesson et al. base their study of Hardangerjøkulen on modeling, as opposed to measurements or observations.
The team used a numerical ice flow model to produce a plausible ice cap history of Hardangerjøkulen thousands of years before the Little Ice Age. Using a modelled history of the ice cap, they examined the sensitivity to different parameters. They found that it is “exceptionally sensitive” to changes in temperature. These changes in temperature impact the ice cap’s surface mass balance, which is the gain and loss of ice from a glacier system.
The possible disappearance of Hardangerjøkulen has many implications, including impacting Norway’s tourism and hydropower industries. 99 percent of all power production in Norway comes from hydropower, which depends on glaciers’ water storage and seasonal water flow. Glaciers help contribute to water reservoirs used for the hydropower, and Norway itself contains nearly half of the reservoir capacity in Europe.
The ice cap is also a popular destination for hiking and glacier walking, as well as for Star Wars fans hoping to visit the location of Hoth scenes.
Local residents have remarked on noticeable differences in Hardangerjøkulen. Grete Hovelsrud, a senior researcher at the Nordland Research Institute and vice-president of the Norwegian Scientific Academy for Polar Research, told GlacierHub that the potential loss of Hardangerjøkulen is “very sad.” She added, “It is such a beautiful place. I skied across it last spring, and it really feels like being on top of the world.”
From KVERT: “The Kamchatka Volcanic Eruption Response Team (KVERT) monitors 30 active volcanoes of Kamchatka and six active volcanoes of Northern Kuriles [both in Russia]. Not all of these volcanoes had eruptions in historical time; however, they are potentially active and therefore are of concern to aviation... In Russia, KVERT, on behalf of the Institute of Volcanology and Seismology (IVS), is responsible for providing information on volcanic activity to international air navigation services for the airspace users.” Many of these volcanoes are glacier-covered, and the interactions between lava and ice can create dramatic ice plumes. Sheveluch Volcano currently has an orange aviation alert, with possible “ash explosions up to 26,200-32,800 ft (8-10 km) above sea level… Ongoing activity could affect international and low-flying aircraft.”
Read more about the volcanic warnings here, or check out GlacierHub’s collection of photos from the eruption of Klyuchevskoy.
New Insights Into Seismic Activity Caused by Glaciers
In Reviews of Geophysics: “New insights into basal motion, iceberg calving, glacier, iceberg, and sea ice dynamics, and precursory signs of unstable glaciers and ice structural changes are being discovered with seismological techniques. These observations offer an invaluable foundation for understanding ongoing environmental changes and for future monitoring of ice bodies worldwide… In this review we discuss seismic sources in the cryosphere as well as research challenges for the near future.”
From TheThirdPole.net: An interview with Chhewang Rinzin, the managing director of Bhutan’s Druk Green Power Corporation, reveals the multifaceted challenges involved in hydropower projects in Bhutan. These challenges include the effect of climate change on glaciers: “The glaciers are melting and the snowfall is much less than it was in the 1960s and 70s. That battery that you have in a form of snow and glaciers up there – which melts in the spring months and brings in additional water – will slowly go away…But the good news is that with climate change, many say that the monsoons will be wetter and there will be more discharge,” said Rinzin.
Check out the full interview with Chhewang Rinzin here. For more about hydropower in Bhutan, see GlacierHub’s earlier story.