A warming atmosphere also warms perennially frozen mountains. The stability of frozen rocks decreases with increasing temperature similar to how butter just taken out of a fridge &nbsp;becomes softer and less resistant to &nbsp;the cutting force of the knife. Thawing frozen mountains means softening them, making them less resistant against gravity, leading to breakage of small to large sections, resulting in rock falls, rock avalanches, and landslides. There is growing concern about <a href="https://nepalitimes.com/here-now/for-destruction-ice-is-also-great-and-will-suffice">the impact of global warming</a> on the stability of icy peaks in mountain ranges around the world, which several recent events in the Himalaya well illustrate. Permafrost is a technical short form of ‘permanent frost’ for frozen ground which remains at temperatures below zero degrees throughout the year.&nbsp; Permafrost is below the surface, is not directly visible, and therefore often escapes the attention of scientists and political authorities. Sophisticated methods must be used to explore it, such as drilling, geophysical soundings, or climate-related modelling.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20240907160944_bbe43b730a10b861f318285a1999a1f6f4d245287618ff49ebfc8e51d154f573.jpg" data-media-id="editor_1" data-image-id="20240907160944_bbe43b730a10b861f318285a1999a1f6f4d245287618ff49ebfc8e51d154f573" data-rendition-name="original" width="4108" height="1000" loading="lazy" alt="The not so permanent frost Page 6-7 #1228 NT"> <figcaption>Even small glacial lakes, such as these currently forming near the terminus of the Kangchenjunga glacier in eastern Nepal, can be dangerous. Photo: ALTON C BYERS(Photo: Shristi Karki)</figcaption> </figure>  Generally, temperatures at surface level and directly below match the temperature of the air immediately above it. Polewards to around 60°N and S latitude, mean annual air and ground temperatures are mostly below 0°C. Permafrost is widespread in Alaska, northern Canada and Siberia. The lower limit of negative mean annual temperatures is at &nbsp;2,000-3,000m at mid-latitudes such as the <a href="https://nepalitimes.com/here-now/in-high-places">European Alps</a> or the Southern Alps of New Zealand, to 3,000-4,000m in the Himalaya, and to 5,000m near the equator in the Peruvian Cordilleras. Above these elevations, permafrost affects peaks. In high mountains the permafrost area is often far larger than their glacier-covered regions. In Nepal, the permafrost-affected area is about 2 to 3 times bigger than the glacier area, while in China with the perennially frozen Tibetan Plateau this factor is about 30. Temperatures decrease by 6-7°C for every 1,000m of altitude increase, and the coldest and most deeply frozen rocks are found in the highest parts of the peaks. The frozen zone inside mountains can reach depths of hundreds of metres. It is not just the ice on peaks in the European Alps or the Himalaya that is frozen throughout the year, but so are the rocks.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20240907160944_b75f78e4ee6d146e797f06536491c445891fbeb578f60105f57247a8dc066bbd.jpg" data-media-id="editor_3" data-image-id="20240907160944_b75f78e4ee6d146e797f06536491c445891fbeb578f60105f57247a8dc066bbd" data-rendition-name="original" width="916" height="674" loading="lazy" alt="The not so permanent frost Page 6-7 #1228 NT"> <figcaption>Mt Chamlang (7,319m) with creeping frozen debris (rock glaciers, yellow arrows) and Lakes 464 and 465 (blue arrows) from glacier retreat at its foot. Mt Makalu (8,485m) is in the background.(Photo: Shristi Karki)</figcaption> </figure>  The sunny side of mountains are warmer, and the permafrost is thinner there than slopes in mountain shadow. Temperatures are not constant throughout the year, so a thin surface layer up to a few metres on top of permafrost that thaws in summer and freezes in winter. This seasonal freezing and thawing surface layer on permafrost is called the ‘active layer’. Deep, long-term freezing influences geomorphic processes inside mountains, drastically changing their properties. Growth of ice in cracks and fissures within solid rock tends to expand already existing openings, and even create new ones. The related weakening of bedrock, however, is compensated by strong adhesion and increasing strength induced by the ice fillings and related cold temperatures. Read also: <a href="https://nepalitimes.com/banner/tracing-past-glacial-floods-in-kangchenjunga">Tracing past glacial floods in Kangchenjunga</a>, Alton C Byers Not only the ice itself, but also rocks, rock-ice, and rock-rock contacts increase their strength with lower temperatures. Perhaps most important is the effect of freezing and ice filling of cracks between rocks containing water. Deep frozen rocks are essentially impermeable to water as an often-decisive factor of stability inside mountain slopes. In the abundant debris masses at the foot of high mountains, deep, long-term freezing causes even more spectacular changes. Formation of ice inside and beyond the pores can create a mixture of ice and debris with ice lenses, enabling such ice-rich frozen masses to slowly creep down the slopes of mountains. Landforms resulting from permafrost creep over past millennia look like lava streams and are called ‘rock glaciers’.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20240907160944_dc86dc2e254de22afefcd3f6c2df76af6c0aab87555f702dc853992987dcb3fc.jpg" data-media-id="editor_5" data-image-id="20240907160944_dc86dc2e254de22afefcd3f6c2df76af6c0aab87555f702dc853992987dcb3fc" data-rendition-name="original" width="1072" height="625" loading="lazy" alt="The not so permanent frost Page 6-7 #1228 NT"> </figure>  Thawing out From long-term temperature measurements in deep boreholes, we know that global temperature increase of the atmosphere during the past about 100-150 years has warmed up mountain slopes down to depths below the surface of about 100m. The effect of this deep warming is the reversal of the freezing and cooling effects. It reduces the strength of rocks or debris with ice and makes them ‘softer’ and more permeable to water. Over the past decades, creep rates of frozen debris in rock glaciers have markedly increased, and the frequency of large rock-ice avalanches from high-mountain permafrost has accelerated. In the Peruvian Andes, two major events from mountain permafrost occurred in 2020 and 2023. Both had volumes of 1-1.5 million m3, reached lakes at the foot of the slope, and produced flood waves. The 2020 Salkantay flood caused loss of lives and heavy damage at Santa Teresa, 35km down valley. The flood wave at Rasac was fortunately retained within the lake at lower altitude. On 5 May 2012, a massive rock, ice, and debris avalanche from Annapurna IV <a href="https://nepalitimes.com/here-now/remembering-the-seti-disaster">cascaded into the Seti River gorge</a>, plummeting into a rockfall-dammed lake. The impact triggered an air blast that levelled thousands of hectares of forests, a dust cloud covered the countryside in fine white rock powder, and a hyper-concentrated slurry flood that killed 72 people downstream.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20240907160944_81860cf5896090449c7fd074796f683c164e2bff782a46390cd43eee6202f19b.jpg" data-media-id="editor_7" data-image-id="20240907160944_81860cf5896090449c7fd074796f683c164e2bff782a46390cd43eee6202f19b" data-rendition-name="original" width="780" height="539" loading="lazy" alt="The not so permanent frost Page 6-7 #1228 NT"> <figcaption>Rock failure from Annapurna IV led to a series of cascading events that resulted in the Seti River flood of 2012 that killed 72 people. Map: J  KARGEL / D REGMI(Photo: Shristi Karki)</figcaption> </figure>  On 20 April 2017, a high altitude breakage of solid rock from the east face of Saldim Peak (6,388m) in the <a href="https://nepalitimes.com/here-now/nepal-s-mountains-are-melting">Barun Valley turned into a 1.1 million m3 debris flow</a> of ice and sediment that plummeted 1,200m down to the Langmale Glacial lake below. Although the lake was less than 0.01km2 in size, the combination of lake water with melting ice from the ice-debris flow triggered a massive hyper-concentrated flood that destroyed forests, pastureland, and trekking lodges for several dozen kilometres to the Barun’s confluence with the Arun. In India’s Uttarakhand state bordering Nepal, the Chamoli event of 7 February 2021 was catalysed by the detachment of 20 to 30 million m3 of rocks and ice from a frozen, ice-clad peak. The ensuing avalanche developed into a rapidly flowing mass of rocks, ice and water, killing 204 people and heavily damaging an under-construction hydropower infrastructure 35km downstream.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20240907160944_c7284846f8a571d8d1f5596b7731e7c4c2521f764aaf9e5df23ad9d0ad41d986.jpg" data-media-id="editor_9" data-image-id="20240907160944_c7284846f8a571d8d1f5596b7731e7c4c2521f764aaf9e5df23ad9d0ad41d986" data-rendition-name="original" width="798" height="462" loading="lazy" alt="The not so permanent frost Page 6-7 #1228 NT"> <figcaption>This massive breakage (below) of solid rock from Saldim Peak in 2017 fell on a lake and unleashed a flood downstream on the Barun River. Top photo is of the peak before the collapse. Photos: ALTON C BYERS(Photo: Shristi Karki)</figcaption> </figure>   <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20240907160944_6e686f290b44e89cce8a1b822a74895c8d6a4ac4122572223ba3c4160b88879f.jpg" data-media-id="editor_10" data-image-id="20240907160944_6e686f290b44e89cce8a1b822a74895c8d6a4ac4122572223ba3c4160b88879f" data-rendition-name="original" width="799" height="470" loading="lazy" alt="The not so permanent frost Page 6-7 #1228 NT"> </figure>  On 3 October 2023, the collapse of about 15 million m3 of debris from a perennially frozen moraine into <a href="https://nepalitimes.com/news/sikkim-flood-is-warning-to-nepal">South Lhonak Lake in the Sikkim</a> Himalaya produced a flood wave and debris flow which killed 14 people with over 100 missing, destroyed a hydropower reservoir at Chungthang, 60km downstream, and caused destruction of houses, roads, and agricultural land. Similar processes may have been involved in the Birendra Tal glacial lake flood of 21 April 2024 and <a href="https://nepalitimes.com/here-now/lives-on-the-line-in-the-himalaya">the Thame flood of 16 August 2024</a>. Each of the above cases show the potential hazard over long distances related to process chains, especially in connection with impacted mobile water bodies in glacial lakes and artificial reservoirs.&nbsp; <h2>12 TIPS: Awareness and Protective Measures</h2> Changes in high altitude permafrost, and the devastating geomorphic events they cause are still poorly understood by Nepal’s scientific community and government. Earthquakes and heavy rainfall are usually reported by the press to be the primary causes of catastrophic events, both of which are impossible to predict. However, climate change and gravity, the two major forces at work on Himalayan permafrost, are constants. As permafrost continues to destabilise at the highest altitudes in the Nepal Himalaya, more and more devastating events can be expected to occur.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20240907160944_dd2d77fb090fb2f5c836411d61bd6e7bb4e2e40ea2abae3d8eee8a686e9457dc.jpg" data-media-id="editor_13" data-image-id="20240907160944_dd2d77fb090fb2f5c836411d61bd6e7bb4e2e40ea2abae3d8eee8a686e9457dc" data-rendition-name="original" width="977" height="733" loading="lazy" alt="The not so permanent frost Page 6-7 #1228 NT"> <figcaption>Gabions installed near Chukung in 2015 protected the village from a similar flood from the Lhotse Glacier in 2014. Photo: ALTON BYERS(Photo: Shristi Karki)</figcaption> </figure>  The question is, what can we do about it? Based on our collective experience in the European Alps, Peruvian Andes, and Nepal Himalaya over the past several decades, we offer the following suggestions: 1. Encourage more permafrost and hazard research. Nepal’s scientists and practitioners need to better understand and acknowledge the role of permafrost change in the growing list of climate change-related impacts in the high mountain environment, and more research of an applied nature is indicated. Interdisciplinary approaches that include and involve local people usually yield the most promising and effective results. 2. Standardise glacial lake risk assessment methods. Currently, scientists use various methods to assess a lake’s potential danger of flooding, with predictably mixed and widely differing results. Imja glacial lake in Khumbu, for example, is considered by some scientists to be extremely dangerous, and by others to have a low to moderate risk. The result is confusion among local people, local governments, and scientists alike. 3. Update and revise the current list of potentially dangerous glacial lakes in Nepal. The inventory should incorporate the changing permafrost factor, including smaller lakes less than 0.01km2. Even very small glacial lakes, such as those above Thame and the Langmale glacial lake in the Barun, can be as destructive as large lakes under the right conditions and cascading processes. 4. Develop new feasibility study protocols for large hydropower projects. These guidelines must incorporate the changing permafrost factor as well as the heightened threat of glacier floods. The potentially disastrous impacts of climate change upon major hydropower projects in Nepal have been predicted by scientists for decades, and yet the construction (and destruction) of major, multi-million-dollar installations continues. Hundreds of lives, and millions of dollars of infrastructure, stand to be saved through the use of more detailed, comprehensive evaluations of permafrost and glacier-related risks prior to project implementation. 5. Develop zoning policies. These should discourage the location of farms and infrastructure (homes, tourist lodges) within known and active floodplains. Some scientists believe that most of the deaths from the 2012 Seti flood could have been prevented had settlements not been located directly in the floodplain. 6. Simple is beautiful. Rock-filled wire cages (gabions) can be engineered to effectively divert floods and should continue to be promoted in high mountain regions. In the village of Chukung located directly in the floodplain of the Lhotse Glacier in the Sagarmatha National Park, for instance, the installation of gabions after a glacier flood in 2015 protected the village the following year when a second similar flood from the same glacier occurred.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20240907160944_ce975f82275c7936c7948fbf7fd7231b61adecc01d5510760144a8f3d0467859.jpg" data-media-id="editor_14" data-image-id="20240907160944_ce975f82275c7936c7948fbf7fd7231b61adecc01d5510760144a8f3d0467859" data-rendition-name="original" width="1005" height="695" loading="lazy" alt="The not so permanent frost Page 6-7 #1228 NT"> </figure>  7. Build higher bridges. This can effectively address the growing frequency and magnitudes of glacier floods in the high mountains, eliminating the need for continuous rebuilding. 8. Increase awareness. Nepal’s mountains will continue to destabilise and become even more dangerous in future. Exercising extra caution while crossing a landslide, an active torrent, or a debris-covered glacier is a fact of life in today’s high Himalayan regions. Likewise, constructing a lodge, school, or community building beneath a small and seemingly harmless glacial lake should be discouraged. 9. Promote simple and effective early warning systems. In spite of their much-touted role in disaster mitigation, early warning systems installed to date at potentially dangerous glacial lakes in Nepal have proven to be expensive disappointments. They are typically installed by a remote and distant government agency, little training in their use by local villagers is offered, and local people say they have no idea what the warning sirens sound like nor what they should do if one goes off. Thus far the most effective and proven EWS tool has been the cell phone. Hundreds of lives were saved during the Seti River flood of 2012 when upstream witnesses phoned warnings to their downstream family and friends. 10. Improve mechanisms that allow scientists to communicate. The results of their permafrost and glacier hazard research should directly, quickly, and effectively be communicated to decision-makers. This has proven to be easy to recommend but difficult to implement in most of the world but is nevertheless in need of our constant efforts to achieve. 11. Encouraging transboundary permafrost research. Increased cooperation between scientists and researchers in Nepal, China, and India is needed to help identify potentially vulnerable crossborder rockfall, avalanche, and catastrophic flooding risk. 12. Develop and implement adaptation planning. Continue planning and training programs targeted at permafrost-related floods and other highland-lowland hazards. Local Adaptation Plans for Action (LAPA) have proven to be an effective tool for increasing local awareness of climate impacts as well as planning for mitigation measures. Dr Wilfried Haeberli is with the University of Zurich and Dr Alton C Byers University of Colorado at Boulder.

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The not-so-permanent frost

Fenerbahçe Beko won the Turkish Airlines EuroLeague finals in Abu Dhabi, held 23-25 May, defeating Monaco 81-70 in the final. Olympiacos, who defeated Panathinaikos 97-93, finished the series in third place. The Most Valuable Player (MVP) of the final match, Nigel Hayes-Davis from Fenerbahçe Beko, received a prize of 1,000,000 Miles&amp;Smiles from Turkish Airlines’ Chief Commercial Officer Ahmet Olmuştur. The carrier has been the title sponsor of the Turkish Airlines EuroLeague, a top tier tournament, since 2010.

Turkish Basketball

While Nepal was hosting the Sagarmatha Sambaad international climate conference in Kathmandu this month, on Mt Everest it was pretty much business as usual.&nbsp; The signs of climate breakdown are all there: a river now runs through Base Camp in summer, the Khumbu Icefall is more unstable, and there are more &nbsp;frequent avalanches. When expeditions arrived in March, the mountains were bare: it had not snowed since September, but then blizzards dumped unseasonal snow in May. And despite climate worries, such is the pull of Himalayan mountaineering that the Everest Industry showed no signs of slowdown. More than 600 international climbers and their Nepali guides had made it to the summit of the world’s highest mountain. At one point there were an estimated 2,000 people in the tent city on the Khumbu Glacier. All the ropes and ladders on the Icefall came down on Thursday, marking the official end of the spring climbing season, and just in time to avoid a monsoon cyclone approaching from the Bay of Bengal. It has been an action-packed season. One factor could be that Everest fees will go up from September: each foreign climber needs to pay a $15,000 royalty, up from the present $11,000. The cost for a Nepali climber on the South Col route will also go up: from Rs75,000 to Rs150,000.&nbsp; The fee to climb Everest in autumn is $7,500 (up from $5,500), but most climbers still prefer spring. Winter permit fee (December-February) is only $3,750 per person and the mountain is now also open for monsoon (June-August) climbs, when the fee is ever lower at $2,750. The revised rule also makes it mandatory for every two climbers on an 8,000m peak to hire one Nepali mountain guide.&nbsp;  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/2025053004050_67f856fe52714e4bdcf21ae7d45c6f18c82117b9d0a5f73ed1efa04c96de1046.jpg" data-media-id="editor_0" data-image-id="2025053004050_67f856fe52714e4bdcf21ae7d45c6f18c82117b9d0a5f73ed1efa04c96de1046" data-rendition-name="original" width="931" height="732" loading="lazy" alt="The Everest Industry graph 1"> </figure>  In addition, climbers also have to pay for porters and guides, equipment, Base Camp costs, Ice Fall and fixed rope team fees, so climbing Everest does not come cheap. But such is the draw of climbing the world’s highest peak that some say the increased fees will not diminish the crowds next year. The government has tried to spread expeditions out to other seasons and other 8,000ers, but with not much success. Earlier this year, Nepal unilaterally increased the number of 8,000m peaks to 14 by adding six more sub-summits to broaden the choice for climbers. Added were: Yalung Kang (8,505m), Yalung Kang West (8,077m) &nbsp;Kangchenjunga Central (8,473m), Kangchenjunga South (8,476m), Lhotse Middle (8,410m) and Lhotse Shar (8,400m).&nbsp; The announcement could go against the accepted topographic criteria that a stand alone peak has to be at least 300m higher than an adjoining prominence, and at more than 3km isolation from it. The UIAA (Union Internationale des Associations d'Alpinisme) still recognises only 14 mountains as eight-thousanders, and only eight of those are in Nepal, or on the border with China. Nepal’s revised mountaineering regulations also increased the insurance coverage of high-altitude workers to protect porters and high altitude guides who usually take more risks on the mountains. Rescue teams and clean-up campaigners to collect trash and remove bodies of dead climbers up to Camp IV of Mt Everest do not need permits.&nbsp; The Sagarmatha Pollution Control Committee is now using drones to fly down trash in 20kg sacks. Each climber is also required to bring down at least 6kg of waste and not just their own, but this rule is erratically enforced. With five fatalities on Everest and Lhotse, Spring 2025 had a historically low death toll. Another five climbers died on Annapurna, Kangchenjunga and Makalu.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/2025053004050_38681de22f0fefb6faa12b01755566d09c5064d0ff84e12ccc7b5d68ea9ba38a.jpg" data-media-id="editor_1" data-image-id="2025053004050_38681de22f0fefb6faa12b01755566d09c5064d0ff84e12ccc7b5d68ea9ba38a" data-rendition-name="original" width="665" height="740" loading="lazy" alt="The Everest industry graph 2"> </figure>  Journalist Ben Ayers who ran the Everest Live social media channel from Everest Base Camp with daily updates credited the low death rate to dramatic rescues of climbers from the ‘Death Zone’ by their Nepali guides and longline helievacs — the visuals all uploaded on YouTube.&nbsp; “Ironically, this perception of safety is bringing more and more inexperienced climbers to the mountain, and they need more rescues,” Ayers said in one of his dispatches.&nbsp; American expedition chronicler and summiteer Alan Arnette suspects there is a lot of under-reporting given that the jet stream and storms were lashing Everest even till late in the season. He told us: “I heard a lot about frostbite and rescues that were not made public. It’s become practically impossible to cover the details on Everest. All the teams report nice news, and they don’t talk about bad stuff to avoid hurting businesses.” Although trash on Nepal’s mountains makes headlines, what does not receive as much attention is the climate impact of so many expeditions. The Sagarmatha Sambaad conference sidestepped this issue, which is ironic given that the impact of climate breakdown is most evident on Himalayan peaks and their glaciers.&nbsp; <h2>Need for Speed</h2> The big stories this year have been about speed-running from their home cities to the top of Everest. Ukrainian entrepreneur Andrew Ushakov flew out of JFK on 15 May at 10:15AM Nepal time, and was on the summit 3 days, 23 hours, and 7 minutes later on 19 May at 9:22AM.&nbsp;  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20250601080640_1c5cc6fc991307861768f07037ed9d30930fb20f35dbb57dc31c9a92a9e1a885.jpg" data-media-id="editor_2" data-image-id="20250601080640_1c5cc6fc991307861768f07037ed9d30930fb20f35dbb57dc31c9a92a9e1a885" data-rendition-name="original" width="1440" height="1800" loading="lazy" alt="The Everest Industry"> <figcaption>Andrew Ushakov at the summt. Photo: ELITE EXPED</figcaption> </figure>  “I could never find the time for the traditional 40-50 days of acclimatisation,” Ushakov explained matter-of-factly. His ‘Everest Sea-to-Summit’ climb was possible because he spent 400 hours in hypoxic sleep tents over the past four years in New York. However, Ushakov did use ropes already fixed, hired four Nepali guides, helicoptered to Base Camp, and used much more oxygen than an average climber. And after the climb, Ushakov was arrested at Kathmandu airport for being in possession of $20,000 of undeclared cash and spent a night in jail and fined $60,000.&nbsp; The other speedsters were Garth Miller, Alastair Cairns, Anthony Stazicker, and Kev Godlington, all former British Army commandos. They left London and summited five days later on 21 May, and flew right back. They also used hypoxic tents to simulate the thin air high on Everest.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20250601080644_90c8dd5cc07b4b43f2989b1dc0c0650ab80f10ebb06680c25a6909c519957bd8.jpg" data-media-id="editor_3" data-image-id="20250601080644_90c8dd5cc07b4b43f2989b1dc0c0650ab80f10ebb06680c25a6909c519957bd8" data-rendition-name="original" width="810" height="668" loading="lazy" alt="The Everest Industry "> <figcaption>All four members of the Furtenbach team at the summit. Photo: Sandro Gromen-Hayes</figcaption> </figure>  But more controversial was their use of xenon gas therapy in a German hospital to ramp up the production of oxygen-carrying haemoglobins in their blood. Xenon is banned by the World Anti-Doping Agency for being performance enhancing in sports. Expedition leader Lukas Furtenbach said this rule does not apply to mountaineering, as it is not a regulated sport like swimming. Nepal has no rules about xenon, but the Department of Tourism said it was launching an ‘investigation’ to decide on future policy since it is difficult to ban xenon, but allow oxygen. The controversy has also divided the mountaineering community, with some climbers saying they just want to maximise their chances of survival. Spending less time on the mountain could make climbing safer by reducing avalanche risk. It would also mean less trash on the mountains, but it would reduce the income of Nepal’s expedition industry. It is also unclear how much of the success was due to xenon therapy and whether the ex-special forces were already in good physical shape.&nbsp; The need for speed hides the fact that climbing in the Himalaya is dangerous business, and climbers cannot sprint to the top just by huffing xenon. But ultra-fast climbs could be charged more, and the revenue generated can be used to establish state-of-the-art rescue operations, and increase pay and insurance for guides. Two other speed chasers this season were Swiss-Ecuadorian Karl Egloff and American Tyler Andrews, both on Everest without oxygen. Andrews choppered to Base Camp to catch a weather window, but turned back from 8,500m due to high winds. Heavy snow and wind also forced Egloff to descend from 7,000m. Slow and steady climbers like Anja Blacha from Germany did make it to the summit without oxygen, while Kami Rita Sherpa broke his own record with his 31st Everest summit as he led a 26-strong Indian Army group. There were 468 permits issued for foreign climbers from 48 expeditions to Everest this spring. Nepal’s other eight-thousanders together had only 17 expeditions. Nepal has more than 1,000 peaks above 6,000m, and has opened only 476 of them for climbing.&nbsp;

The Everest Industry

While Nepal marked <a href="https://nepalitimes.com/news/mt-everest-pvt-ltd">Mt Everest</a> Day on 29 May, on the other side of the planet in the US state of Colorado dozens of Nepalis who have climbed the world’s highest peak multiple times were busy working as chefs and Uber drivers. Among them is Nima Doma Sherpa, who climbed Mt Everest in 2019 after her husband Tshering Wangchu was among 16 crushed by an avalanche on <a href="https://nepalitimes.com/banner/on-thin-ice-in-the-khumbu">the Khumbu Icefall</a> five years earlier. A large serac broke off the West Shoulder of <a href="https://nepalitimes.com/news/the-everest-industry">Mt Everest </a>and fell directly on a group of <a href="https://nepalitimes.com/opinion/more-porters-sick-on-everest-trail">porters and guides</a> making their way up the Icefall at 5,800m. Their bodies were flown by helicopter to Khumjung where Tshering Wangchu was born. He was excited about climbing Mt Everest for the first time.&nbsp; In Khumjung, Nima Doma felt like her own life had also ended. This was the kind of news Sherpa wives, mothers and sisters dreaded every <a href="https://nepalitimes.com/here-now/peak-climbing-season-2025-s4abrxny">mountaineering season</a>. She stayed home for more than two years grieving, but ultimately gathered up all her emotional strength to take care of her 6-year-old son and 3-year-old daughter. Nima had grown up in Khumjung hearing <a href="https://nepalitimes.com/review/stories-of-nepal-s-summiteers">tales of adventure on the mountains </a>from their father, Ang Chubi Sherpa who had climbed Everest in 1993. He used to bring her and her sisters and brother European chocolates after every expedition, and used to tell them that the chocolate bars grew on the mountains. “It was only after we got older did we realise that he told us that chocolates grew in the mountains so we would not worry about him putting himself in harm's way,” Nima Doma recalled with a faraway look at her home in Boulder this week. Nima went to the school that <a href="https://archive.nepalitimes.com/article/Nepali-Times-Buzz/commemorating-edmund-hillary-in-nepal,4145">Edmund Hillary</a> opened in Khumjung till Grade 8, and then dropped out to help in the kitchen and <a href="https://nepalitimes.com/here-now/when-yaks-go-so-does-culture">tend yaks</a>. She was married off to Tshering Wangchu, who was also a high altitude guide. When Tshering went on expeditions, Nima also started working as a porter from Namche to Base Camp. It was perhaps her father’s tales of mountains of chocolates that had always attracted her to <a href="https://nepalitimes.com/here-now/knowing-our-mountains-43v4iyvo">the peaks</a>. After her husband was killed ten years ago this month, being a widow with children was not easy for Nima Doma. But she was not alone: there were at least 200 single mothers in <a href="https://nepalitimes.com/here-now/khumbu-since-1950-jaww4qn0">the Khumbu</a>, and 20 of them just in Khumjung whose husbands had been killed in <a href="https://archive.nepalitimes.com/article/nation/tragic-start-to-himalayan-spring-nepal,3695">mountaineering accidents</a>. Some were not even 20 years old, and had children growing up without fathers. But there were also women in the 50s whose husbands had been killed in the 1980s. Nima found sponsors for her children’s education, and moved to Kathmandu. In the capital, Sherpa widows used to meet to help each other. Some of them had joined the Nepal Mountaineering Association (NMA) training for rock and ice climbing. “I decided that it was no use sitting home and crying anymore, after meeting other single mothers I felt less alone,” remembers Nima, who joined the Juniper Foundation and enrolled in an NMA training camp in Manang. There she climbed Chulu East (6,584m) and met Furadiki Sherpa, whose rope-fixing husband had also been <a href="https://nepalitimes.com/news/on-mt-everest-s-70th-records-and-fatalities">killed on Everest</a> in 2013. They set themselves the goal of climbing Everest one day, and started a fund-raising drive.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20250530090544_621be0724b9182c8e3594b2c562a71ec32ac01d985a71d0cf31646de9d51e15a.png" data-media-id="editor_12" data-image-id="20250530090544_621be0724b9182c8e3594b2c562a71ec32ac01d985a71d0cf31646de9d51e15a" data-rendition-name="original" width="2678" height="1274" loading="lazy" alt="Everest summiteers find new life in the US"> </figure>  “We decided we had to overcome society’s stigma of <a href="https://archive.nepalitimes.com/article/nation/widows-personal-happiness-comes-last-in-face-of-social-financial-hardships,1855">widowhood</a> and prove that <a href="https://nepalitimes.com/here-now/remembering-junko-tabei">women could also climb mountains</a>,” Nima said, adding that she was inspired by Nepal’s first woman Everest summiteer Pasang Lhamu Sherpa, who died during her descent in 1993. Nima Doma and Furdiki climbed the technically-difficult Ama Dablam (6,812m) and then arrived at Everest Base Camp in April 2019 as part of their Two Widows Expedition with the motto, ‘So Can We’. While climbing up the Icefall Nima passed the spot where her husband had been killed. It was a jumble of constantly-shifting ice blocks bigger than houses. She closed her eyes and said a prayer. “I remember thinking, this is so difficult and dangerous. This is what my husband had to do to support our family,” Nima Doma said. “I was determined to fulfil my husband’s dream of climbing Chomolungma, and to prove to ourselves that we two women could do it.” It was 23 May 2019 when <a href="https://www.reuters.com/article/world/two-sherpa-widows-scale-everest-and-smash-stigma-idUSKCN1SU0MV/" target="_blank">Nima and Furdiki stepped on the summit</a> and looked over into Tibet, and down at Tengboche Monastery to the south.&nbsp;  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20250530090544_6b822582b5d88ba5e972db084f184690b40653c6efd9901b2dd082ffba2a263b.png" data-media-id="editor_16" data-image-id="20250530090544_6b822582b5d88ba5e972db084f184690b40653c6efd9901b2dd082ffba2a263b" data-rendition-name="original" width="2700" height="1522" loading="lazy" alt="Everest summiteers find new life in the US"> </figure>  Nima Doma hugged Furdiki, took off her mask and wept. But for the first time in five years, it was not from grief but relief — relief for being free of all the sadness and sacrifices and for fulfilling her husband’s dream. They had found <a href="https://nepalitimes.com/here-now/life-after-death">life after death</a>. “I felt this immense joy to be on top of the world, it was indescribable,” Nima Doma said, “I have wept only twice in my life. Once when my husband died, and once there on top of Everest.” The tears had frozen on Nima Doma’s cheeks, as she and Furdiki headed back down the mountain.

Everest summiteers find new life in the US

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The Everest Industry

Everest summiteers find new life in the US

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