The<a href="https://nepalitimes.com/news/rasuwa-flood-likely-a-glof"> flood on the Bhote Kosi</a> on Tuesday morning was a timely reminder about the risks Himalayan communities face from melting permafrost and glaciers, as well as the need for transboundary early warning. In the spring of 2024, I visited the Kanchenjunga Conservation Area (KCA) again. While in the village of Kampuchen (4,145) I visited Nupu Sherpa, friend and owner of the Kampuchen White House Lodge, to share <a href="https://tc.copernicus.org/articles/18/711/2024/">a new paper we had just published</a> about a massive ice-debris avalanche that had occurred in 2022 in the upper Nupchu valley. Although Nupu was interested in the results and implications of the avalanche, he was even more concerned about the recent and rapid development of several large, pro-glacial lakes upon the terminus of the Kanchenjunga glacier, an hour walk north of Kampuchen and across the seasonal yak pasture of Ramdang Kharka (4,375m).&nbsp; Like many high altitude, low gradient glaciers in the Himalaya, those in the Kanchenjunga region had shrunk to mere shadows of their former selves during the previous 125 years, leaving behind debris-covered remnant ice and small meltwater ponds.&nbsp; Nupu’s fear was that the lakes might soon coalesce to form a large and potentially dangerous glacial lake. Given a large enough trigger, such as a massive landslide or avalanche, a glacial lake outburst flood (GLOF) could result that could damage Kampuchen, Ghunsa, Phale, the Kangchenjunga Base Camp trail, and even beyond to the lower Tamor into India.&nbsp;  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/2025071204070_31e28d1fd0f5a976ad96fc5597cc386586d7de5b7d9714835d5b479104209fed.jpg" data-media-id="editor_2" data-image-id="2025071204070_31e28d1fd0f5a976ad96fc5597cc386586d7de5b7d9714835d5b479104209fed" data-rendition-name="original" width="1500" height="1635" loading="lazy" alt="Meltpools in the Himalaya"> <figcaption>The Kanchenjunga Conservation Area (KCA), eastern Nepal.</figcaption> </figure>  Since I was on my way to the village of Lhonak (4,792m) I stopped to take a look at the new lakes. Sure enough, from a lookout point on the lateral moraine of the Kanchenjunga Glacier I could see as many as ten newly formed and growing meltwater ponds upon the terminal moraine region of the glacier.&nbsp; The prospect was reminiscent of early satellite images taken of Imja Glacier in 1962 by the French, showing a number of meltwater ponds that within 15 years had grown and merged into a glacial lake half a square kilometer in size and containing 45 million cubic meters of water. Ten years after that Imja had grown to more than a square kilometer in size, was at least 120 m deep, and contained an estimated, and growing, 90 million cubic meters of water. Would the same scenario play out for the lower Kanchenjunga Glacier? To try and understand the situation better, glaciologist Sonam Wangchuk of ICIMOD put together a time series composite of lake development over time, from 2016 to 2024, where it was clear that the majority of the new lakes had only formed since 2019.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/2025071204078_c65a5ec574a251489c502f3efdf842033e0d238fd57947f7eee2c5793aac2a29.jpg" data-media-id="editor_3" data-image-id="2025071204078_c65a5ec574a251489c502f3efdf842033e0d238fd57947f7eee2c5793aac2a29" data-rendition-name="original" width="602" height="686" loading="lazy" alt="Meltpools in the Himalaya"> <figcaption>Time-lapse satellite images of glacial lake development from 2016 to present. Animation of the process can be seen at https://www.mdpi.com/article/10.3390/w17101457/s1.</figcaption> </figure>  Sonam Rinzin of Newcastle University estimated the potential depth and volume of the future glacier lake using standard procedures based upon the surface slope of the Kanchenjunga Glacier combined with volume-area curves for similar glacial lakes, estimating that the future lake would have a volume of approximately 33 million cubic meters of water and depth of more than 116 m. Other modeling methods enabled the mapping of probable ice, debris, and/or rock avalanches into the lake that could trigger a GLOF.&nbsp; A third model was then used to simulate four different avalanche scenarios that could trigger a GLOF: from small (debris avalanche of 3 million cubic meters) to the worst case (15 million cubic meters) of fast-moving debris. Even under the small magnitude scenario, avalanche-triggered outburst floods would travel distances of almost 120km downstream, and under the worst-case scenario the floods would reach the Indo-Gangetic Plain and cross the border into India, damaging or destroying up to 90 buildings and 44 bridges. The prospective triggers of a future GLOF, however, are not limited to a nearby rock avalanche. A <a href="https://tc.copernicus.org/articles/11/443/2017/tc-11-443-2017.html">sudden release of water</a> from water-filled caves further up the glacier could trigger a surge wave capable of breaching the terminal moraine complex holding in the lake water.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20250712040716_20ed87368a9ac416b5d0232cf8e02211195ca6bc9fff960a1f7e43a95bdfbbf9.jpg" data-media-id="editor_5" data-image-id="20250712040716_20ed87368a9ac416b5d0232cf8e02211195ca6bc9fff960a1f7e43a95bdfbbf9" data-rendition-name="original" width="1500" height="1621" loading="lazy" alt="Meltpools"> <figcaption>Theoretical Kangchenjunga glacial lake of the future (blue) contained by a front moraine (purple) with a flood possibly triggered by a massive rock avalanche (red).</figcaption> </figure>  <a href="https://nepalitimes.com/multimedia/the-not-so-permanent-frost">Weakening permafrost</a> at the highest altitudes could result in massive ice-debris avalanches, such as those believed to have triggered recent and catastrophic floods in the <a href="https://nepalitimes.com/here-now/remembering-the-seti-disaster">Seti River</a>, <a href="https://nepalitimes.com/here-now/nepal-s-mountains-are-melting">Barun Khola</a>, <a href="https://nepalitimes.com/news/non-climate-cause-of-nanda-devi-flood">Chamoli</a>, <a href="https://nepalitimes.com/news/sikkim-flood-is-warning-to-nepal">South Lhonak lake</a>, and Tuesday’s Bhote Kosi flood in <a href="https://nepalitimes.com/news/rasuwa-flood-likely-a-glof">Rasuwa</a>. Weakening and eventual collapse of the terminal moraine complex through sub-surface piping could also result in an outburst flood. And a range of <a href="https://nepalitimes.com/here-now/nepal-s-mountains-are-melting">cascading processes</a> currently unknown to scientists could trigger a flood as well.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20250712040712_76336a4597c08dd735e57b09ae9840b6bd3d89c85907bb39424d9e6f3163581e.jpg" data-media-id="editor_13" data-image-id="20250712040712_76336a4597c08dd735e57b09ae9840b6bd3d89c85907bb39424d9e6f3163581e" data-rendition-name="original" width="740" height="565" loading="lazy" alt="Meltpools in the Himalaya"> <figcaption>Jannu glacier in 1899. Note how the level of the debris-covered glacier reached the top of the lateral moraines over a hundred years ago. Photo: V. SELLA</figcaption> </figure>   <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20250712040712_707dd365923a002e889c64a88796b445695ea9ca692ec639179bc70217ed63c5.jpg" data-media-id="editor_14" data-image-id="20250712040712_707dd365923a002e889c64a88796b445695ea9ca692ec639179bc70217ed63c5" data-rendition-name="original" width="5184" height="3888" loading="lazy" alt="Meltpools in the Himalaya"> <figcaption>Jannu glacier in 2022. The remaining debris-covered glacier is now several hundred meters below the crests of the lateral moraines. Photo: E. BYERS</figcaption> </figure>  But will a large and potentially dangerous glacial actually form at the Kanchenjunga glacier? There’s really no way to tell at this point, although the rapid development of lakes since 2016 is a strong indicator that a large lake is in the process of forming. And rather than wait and see, our current uncertainty does not diminish the need for a more proactive approach to the development of a large glacial lake at some point in the near future. For example, the lower Kanchenjunga Glacier clearly needs to be regularly monitored over the coming years to keep track of glacial lake growth and potential hazards. This could be done by the Department of Hydrology and Meteorology (DHM), ICIMOD, or Kathmandu University with results regularly shared with local people and local governments.&nbsp; In fact, such a service could be developed into a program that is offered to other communities throughout highland Nepal who experience similar situations of glacial lake development, growth, and prospective danger, especially since most communities presently feel that they have no one to turn to for similar information. Inexpensive, locally appropriate, user-friendly early warning systems (EWS) need to be developed for the Kanchenjunga region now, instead of waiting for a tragedy to happen. While the different options and costs are being assessed, the installation of new cell towers in the upper Ghunsa Khola would assure that local residents have access to one of the most effective and proven EWS systems available: cell phones, combined with a lake level monitoring device that broadcasts data and connects to cell phone alarm systems.&nbsp; For example, hundreds of lives were saved when upstream witnesses called their family and friends downstream to warn them of the <a href="https://archive.nepalitimes.com/article/nation/Anatom-of-a-Himalayan-tsunami,1330">Seti River flood</a> near Pokhara in 2014. New zoning policies that prohibit the construction of lodges and other infrastructure in high-risk floodplain regions need to be developed now. Where the infrastructure already exists, villages should be encouraged to install gabion rock-filled wire cages along susceptible river channel or river interfaces to divert the flow of water during a flood event, a method used successfully in both highland and riverine Nepal. Local and national hazard training and response programs need to be developed now. Several examples of excellent programs developed by different organisations in the upper Khumbu region exist that provide excellent models, such as those tested by the US Agency for International Development <a href="https://www.hillarymedal.com/Khumbu-Nepal-Local-Adaptation-Plan-of-Action-%20report.pdf">(USAID) and ICIMOD</a> between 2011 and 2015. Glacial lake reduction&nbsp; Nepal was recently awarded a $36.1 million award by the Green Climate Fund (GCF) to directly confront many of hazards from glacial lake outburst floods jointly implemented by the United Nations Development Programme (UNDP) and the DHM building on past successes at Tso Rolpa and Imja Lakes. There are some lessons learned over the past decades of field work based in Nepal and Peru: 1. The DHM wants to use the project to reduce GLOF risks in Kosi and Gandaki basins and glacial lake reduction programs are planned for Thulagi, Lower Barun, Lumding Tsho, and Hongu 2 glacial lakes.&nbsp; However, the planned lowering depth for Tso Rolpa in 2000 was 20m, with the project ending once 3m lowering was achieved due to lack of funds. Imja lake, which scientists also determined needed to be lowered by at least 20m, was in fact lowered by 3m in 2016 ‘because that’s what they did at Tso Rolpa’.&nbsp; If glacial lake reduction programs are to be implemented under the GCF program they should be based upon good science, and lowered to an effective depth, otherwise the activity will be a waste of funds. <a href="https://sinia.minam.gob.pe/sites/default/files/siar-%20ancash/archivos/public/docs/usaid_glacial_lake_handbookrfs_0-ilovepdf-%20compressed_0.pdf">Peru offers experience</a> for glacial lake lowering. 2. Although large glacial lakes (more than 1sq km) will always command the most media and even scientific attention, it has become abundantly clear in recent years that even small glacial lakes can be just as deadly, given the correct sequence of cascading events, rainfall, snowmelt, and/or other triggers.&nbsp; The 2017 <a href="https://link.springer.com/article/10.1007/s10346-018-1079-9">Barun flood</a> and September 2024 <a href="https://www.stimson.org/event/the-%20thame-glof-disaster-climate-related-disaster-risk-management-in-the-high-himalayas/">Thame flood</a> are two excellent examples. Methods for assessing the flood risk of glacial lakes will need to be revised accordingly to include many of these smaller glacial lakes as well, in addition to the 21 large lakes already considered to be dangerous. 3. Existing and expensive EWS might benefit by some consideration of cheaper, more local, and possibly more effective alternatives. In 2015, for example, <a href="https://digitalcommons.macalester.edu/himalaya/vol37/iss2/7/">villagers</a> living below Tso Rolpa complained that they had no idea how the recently installed EWS worked, what it sounded like, and what to do in the event that it went off. With improved cell service and real-time lake level monitoring apps, local people could check on the lake whenever they wished, as opposed to waiting for some kind of communication from Kathmandu. 4. The GCF grant has the opportunity to become the ‘go to’ place for communities throughout highland Nepal to report any of their concerns related to glacial lakes and/or other observed cryospheric processes. This service could facilitate local people’s ability to adapt to, mitigate, or prevent a range of climate change-related hazards largely unknown to previous generations. Alton C Byers is a faculty research scientist at the Institute of Arctic and Alpine Research (INSTAAR) University of Colorado at Boulder and has visited the KCA including a six-month residency in Ghunsa supported by the Fulbright Nepal Scholar Program. This article is largely based on Evolution of a Potentially Dangerous Glacial Lake on the Kanchenjunga Glacier, Nepal, Predictive Flood Models, and Prospective Community Response. <a href="https://doi.org/10.3390/w17101457">Water</a>, 2025. (Byers AC, Rinzin S, Byers E, Wangchuk S.)

original

674x448

610x380

500x500

400x266

400x240

400x203

301x200

1250x600

1084x550

thumbnail

viewImage

Meltpools in the Himalaya

The sudden and massive flood on the Bhote Kosi early Tuesday morning washed away a strategic bridge on Nepal’s main border crossing with China for trade, tourists and pilgrims. Slurry from the nearly 10m high debris flow left 9 dead and 20 missing, 12 of them Nepalis and six Chinese nationals, and 150 others were rescued by helicopter.&nbsp; Four <a href="https://nepalitimes.com/banner/climate-smarter-himalayan-infrastructure">hydropower plants</a> Rasuwagadi, Trisuli III, Trisuli, &nbsp;Benighat and the Trisuli substation sustained heavy damage, knocking &nbsp;out 230MW of Nepal’s power supply – approximately 8% of the total. Over 100 cargo trucks and new electric vehicles parked at &nbsp;Timure Dry Port were swept away. Read also: <a href="https://nepalitimes.com/news/mapping-kangchenjunga-glacial-flood-risk">Mapping Kangchenjung glacial flood risk</a>, Gabe Allen Officials had initially thought &nbsp;the Bhote Kosi had flooded due to heavy rain in Tibet. However, the Department of Hydrology and Meteorology (DHM) and the National Disaster Risk Reduction and Management Authority (NDRRMA) now say a <a href="https://nepalitimes.com/here-now/living-below-nepal-s-melting-mountains">Glacial Lake Outburst Flood (GLOF)</a> is likely.&nbsp; NDRRMA spokesperson Suresh Sunar said it was too early to tell which one, but the flood was most likely the result of one of the glacial lakes in Tibet. Bhote Kosi begins on the north slope of the Ganesh Himal near the Nepal-China border, and its tributary Lende drains the catchment area north of Langtang. The slurry flood on Tuesday was on the Lende (map).&nbsp;  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20250709110720_bbc99c5f3e3d61a3d340892e0273fee3605a8d334a2beb354126137bcf0c8d27.jpg" data-media-id="editor_3" data-image-id="20250709110720_bbc99c5f3e3d61a3d340892e0273fee3605a8d334a2beb354126137bcf0c8d27" data-rendition-name="original" width="629" height="759" loading="lazy" alt="Bhote Kosi flood map"> </figure>   <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20250709110720_39e2f574ff8c12cecda2e5a999d2ba8a0310f599f6b2261dcad7dd43f94df2a1.jpg" data-media-id="editor_4" data-image-id="20250709110720_39e2f574ff8c12cecda2e5a999d2ba8a0310f599f6b2261dcad7dd43f94df2a1" data-rendition-name="original" width="997" height="613" loading="lazy" alt="Bhote Kosi flood map"> </figure>  “Preliminary study suggest that the disaster was not caused by rain in Tibet, but by a glacial lake burst, or another accident,” said Kamal Ram Joshi of the DHM. The level of water at a self-monitoring station in Timure in Rasuwa increased by 3.5m at 3:10AM on Tuesday morning while 13km downstream in Syabrubesi, the level rose by 3.65m at 3:30AM. The same station recorded 5.37m ten minutes later, after which it stopped giving a reading, possibly because the station was also washed away. The flood reached <a href="https://nepalitimes.com/here-now/neither-side-lost-both-sides-won">Betrawati</a> by 5AM, and some of the debris flow reached Mugling during Tuesday. DHM’s Flood Forecasting Division noted that there was no major precipitation in the Bhote Kosi watershed in Nepal and China in the 24 hours preceding the flood.&nbsp;  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20250708100724_313a684b65fc5317064779e47409a40f2bbce2c0c84db995e7f8fc6e1c142105.jpg" data-media-id="editor_6" data-image-id="20250708100724_313a684b65fc5317064779e47409a40f2bbce2c0c84db995e7f8fc6e1c142105" data-rendition-name="original" width="3600" height="1662" loading="lazy" alt="Bhotekosi flood"> <figcaption>The Miteri bridge before it was swept away by the flood in Bhotekosi on the Nepal-China border. Photo: SUBASH DHUNGANA / RSS</figcaption> </figure>   <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20250708100732_ec43f13bae979f7b61bc0db939db4157dc93d3f0767ed527f564bd5c3d12be27.jpg" data-media-id="editor_7" data-image-id="20250708100732_ec43f13bae979f7b61bc0db939db4157dc93d3f0767ed527f564bd5c3d12be27" data-rendition-name="original" width="720" height="432" loading="lazy" alt="Bhotekosi flood NT 2"> <figcaption>The bridge after the flood.</figcaption> </figure>  On Wednesday, several remote-sensing experts using Copernicus &nbsp;satellite images pinpointed the cause of the flood to Purepu Cangbu where supraglacial ponds had merged in June to form a large lake which did not burst, but overflowed &nbsp;and found a channel through englacial conduits to the headwaters of the Lende. The river meets the Bhote Kosi at the Nepal-China checkpoint in Rasuwa.&nbsp; “Analysis of weather forecasts and satellite data shows the Tibet region did not receive enough rain to cause this scale of flooding,” explained Binod Pokharel, associate professor of hydrology and meteorology at Tribhuvan University. “The flood could have been caused by a GLOF."&nbsp; Two weeks ago, Chinese officials had reportedly warned the Rasuwa District Administration in Nepal to be on high alert for floods on rivers that originate in Tibet. It could be that Chinese scientists had observed the alarming<a href="https://nepalitimes.com/here-now/the-climate-crisis-is-a-water-crisis-in-the-himalaya"> expansion of glacial lakes</a> in the Lende and Bhote Kosi catchments. If that was the case, it is an example of the kind of trans-boundary forewarning that would be critical to save lives in future.&nbsp;  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20250708100736_1710142917b30d4f85b343ed52743554d723db918c708f0bade8a0491ba999b2.jpg" data-media-id="editor_9" data-image-id="20250708100736_1710142917b30d4f85b343ed52743554d723db918c708f0bade8a0491ba999b2" data-rendition-name="original" width="1001" height="500" loading="lazy" alt="Bhotekosi flood"> </figure>  However, Rasuwa’s Assistant Chief District Officer Dhruv Prasad Adhikari seems to have no knowledge of any warning from the Chinese side, either formally or informally. &nbsp; “The Chinese Embassy has said the cause of the flood is unknown that it will coordinate with Nepal to find the cause," Adhikari told us. Chinese Ambassador Chen Song and Prime Minister Oli visited the border on Tuesday (pictured). &nbsp; The sharing of real-time trans-boundary rainfall and river flow data would be crucial in early warning about the <a href="https://nepalitimes.com/news/mapping-kangchenjunga-glacial-flood-risk">risk and consequences of GLOFs</a> to reduce human and material loss. But Nepali officials say China has been reluctant to share weather-related information and data not just in this disaster, but in the past as well. “There is no mechanism or system in place for us to obtain hydrological and meteorological data of the Tibetan region,” said DHM Director General Joshi. The <a href="https://nepalitimes.com/here-now/for-destruction-ice-is-also-great-and-will-suffice">Himalaya is melting twice as fast as the rest of the world</a> due to a phenomenon called ‘elevation dependent warming’, and receding glaciers have led to an increasing number of transboundary GLOFs.&nbsp; According to <a href="https://nepalitimes.com/here-now/danger-nepal-s-glacial-lakes-are-filling-up">a 2018 ICIMOD study</a>, of the 47 of the most dangerous lakes that threaten Nepal, 25 are on glaciers in China, 21 in Nepal and one in India. Many of these glaciers are expanding rapidly due to global warming. One of the authors of the report, glacial lake expert Samjwal Bajracharya, says that the report was prepared based on data from 2015. But climate change has accelerated since then. Moreover, seismic activity has further destabilises the landscape, adding to <a href="https://nepalitimes.com/here-now/nepals-glacial-lakes-in-danger-of-bursting">GLOF risk</a>.&nbsp; “Considering the rapid rate of snowmelt and consequent increase in size of Himalayan glaciers, studies should be conducted every year, and a monitoring system should be set up on the glaciers,” says Bajracharya. “However, no studies have been conducted in the Himalaya in a decade, which has been our biggest weakness.” &nbsp;

Rasuwa flood likely a GLOF

Recent outrage in Sikkim over an Indian Army expedition climbing <a href="https://nepalitimes.com/here-now/saving-kangchenjunga">Kangchenjunga</a>, the world’s third-highest peak, has spiked attention to the need to balance mountaineering jobs with indigenous reverence for sacred landmarks. Kangchenjunga (8,586m) is not a peak as much as it is a mountain range with 16 peaks above 7,000m on the border between India and Nepal -- the word itself means ‘five treasures of the snows’ in Tibetan. Some of the highest prominences like Kangchenjunga West and Kangbachen are in Nepal, while the Main, Central and South Peaks are on the border. Climbing the peak from the Indian side has been banned since 2001 because the indigenous Lepcha community there regard the mountain as the abode of Dzoe-nga, the patron deity of Sikkim, which was an independent Himalayan Kingdom until it was annexed by India in 1975.&nbsp; Buddhists in Sikkim say their saint, Padmasambhava, recognised the mountain as a protective spirit. The state has declared the base of the mountain Kangchenjunga National Park, which covers an area one-third of Sikkim. ‘The act of scaling this sacred peak is not only a matter of serious concern but also a violation of both the prevailing legal provisions and the deeply held religious beliefs of the people of Sikkim,’ read a letter from Chief Minister Prem Singh Tamang (Golay) to Amit Shah, India’s Minister of Home Affairs and Cooperation.&nbsp; Tamang continued: ‘We further request Your Honour to take up the issue with the Government of Nepal to ensure that no future expeditions are permitted on the sacred mountain, in deference to the deeply held beliefs and cultural values of the people of Sikkim.’ Kangchenjunga was climbed for the first time exactly 70 years ago by a British team who told King Tashi Namgyal, the Choegyal of Sikkim, that they would not set foot on the summit. Since then, there have been about 532 successful climbs of the peaks and 52 have died while trying.&nbsp;  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20250628060616_5c268e08cf49f36b79ef9b31933fc2d9bf9a6f65414e7ca06dd028bf04e7ccc1.png" data-media-id="editor_1" data-image-id="20250628060616_5c268e08cf49f36b79ef9b31933fc2d9bf9a6f65414e7ca06dd028bf04e7ccc1" data-rendition-name="original" width="1782" height="1178" loading="lazy" alt="Kangchenjunga: too sacred to climb NT"> <figcaption>Indigenous communities in Sikkim held purification ceremonies following the Indian expedition to Kangchenjunga. Photo: THE VOICE OF SIKKIM / FACEBOOK</figcaption> </figure>  <a href="https://nepalitimes.com/here-now/peak-climbing-season-2025-s4abrxny">This spring climbing season</a> alone, there were 70 climbing permits for foreigners issued for Kangchenjunga by the Nepal government, and made it to the top while one French climber died.&nbsp; One of the expeditions this year was an Indian Army team led by Col Ranveer Jamwal, who has summited the highest peaks on all seven continents, and Mt Everest thrice. Jamwal’s team was on the final leg of a ‘<a href="https://economictimes.indiatimes.com/news/india/nimas-summits-mt-kangchenjunga-concludes-historic-har-shikhar-tiranga-mission-successfully/articleshow/121341315.cms?from=mdr">Har Shikhar Tiranga</a>’ (The Tricolour on Every Peak) mission to plant the Indian flag at the highest points of each of India’s 28 states. Kanchenjunga was the last peak they had left, and the hardest, but the expedition put five climbers on the summit. What seems to have incensed the Sikkimese is that while it has banned climbing the mountain from its side, it was an Indian military expedition that went to Nepal to climb the mountain. After news broke of the climb in May, the Sikkim Indigenous Lepcha Tribal Association asked people to observe purification ceremonies in temples across the state. Mayalmit Lepcha of the association acknowledged that the Sikkim government was also partly at fault: “I don’t think such an expedition could have gone forward without the state government being informed, so it could have done something to intervene. It shows weakness. What’s done is done, all we can do is carry out these sanctification ceremonies.”&nbsp; In 2000, one year before Sikkim’s ban, the state allowed an Austrian team to attempt Kanchenjunga’s northeast face for a fee of $20,000, on agreement that they would stop 10m before the summit. Despite this, there was outrage over the expedition on the grounds that it violated Indian laws regarding the defiling of religious sites and Sikkim’s rights to maintain its culture after merging with India. The Indian Army expedition was also seen to have circumvented Sikkim’s law and violated religious sensibilities by going through Nepal. While the team may have thought they were respecting Sikkim’s beliefs by finding a way to complete the mission, the people of Sikkim saw it as defilement.&nbsp; The somber mood of the Sikkim people at the ritual contrasts sharply with Jamwal’s sense of accomplishment. “Without a doubt, the most difficult summit of my life,” he told reporters after the climb. “It tested every ounce of our will.”&nbsp;  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20250628060616_ccfe079c78dab788d19fe2080ee8a5d5dcb11de4157316f6d94e5964da097157.jpg" data-media-id="editor_4" data-image-id="20250628060616_ccfe079c78dab788d19fe2080ee8a5d5dcb11de4157316f6d94e5964da097157" data-rendition-name="original" width="787" height="377" loading="lazy" alt="Kangchenjunga: too sacred to climb NT"> <figcaption>Prayer flags along the Sikkim-Kangchenjunga trekking route. Photo: TREKKINGININDIA.COM</figcaption> </figure>  The <a href="https://nepalitimes.com/news/the-rise-and-fall-of-nims-purja">controversial Nepali-British mountaineer Nirmal Purja</a> was also on Kangchenjunga this spring the mountain, on a mission to summit all 14 8,000m peaks for a third time. He echoed Jamwal about the tough conditions: “The conditions above camp were extremely tough, with deep snow and challenging terrain—more crevasses than usual.” Nepal’s government has not said anything publicly, but it is unlikely that it will ban climbing on Kangchenjunga, since it is becoming popular with expeditions because of its technical challenges, and overcrowding on Mt Everest. Nepal does have bans in place for some of its mountains out of respect for local beliefs. <a href="https://nepalitimes.com/banner/to-open-machapuchre-for-mountaineering-or-not">Mt Machapuchre</a> (6,990m) the imposing pyramid that looms over Pokhara, for example, is seen as an icon of purity by the Gurung people and a symbol of Vishnu by the Hindu communities who live at its base. A strict climbing ban has been in place since 1957, when a British expedition led by Col Jimmy Roberts stopped 45m short of the summit – either because the last bit was too difficult or out of deference to local sentiments.&nbsp; Khumbila that stands above Namche Bazar is only 5,761m high, but like Kanchenjunga is considered the protector deity of the Sherpa people. Gauri Shankar on the Nepal-China border, called Chomo Tseringma by the local community, was off-limits between 1965 and 1979 due to its association with Lord Shiva and Gauri, his consort. Although expeditions are now allowed, there are not too many takers. In Tibet, climbing Mount Kailash is prohibited by the Chinese government because it revered by the Hindus, Buddhists and followers of the Bon faith. Even Mt Everest is regarded as sacred, and its Sherpa name is Chomolungma, Goddess Mother of the Earth.&nbsp; Economically, climbs on Kanchenjunga bring in decent revenue. This climbing season, the 41 permits, at $1,800 each, brought in $73,800. This is somewhat comparable to Makalu, Lhotse, and Annapurna I, but these numbers are dwarfed by the $4 million in <a href="https://nepalitimes.com/news/the-everest-industry">Everest permits</a>. Revenue from Kanchenjunga climbing permits is something Nepal could potentially forgo if necessary, but the expeditions also provide jobs to hundreds of high altitude guides, porters, base camp support staff and other logistical costs.&nbsp; As the third highest mountain in the world and the tallest in India, there will always be significant motivation to climb it from the Nepal side, especially as climbers are drawn by the technical climbing at high altitude.

Kangchenjunga: too sacred to climb?

In 2023, northern India suffered record-breaking heat. In 2024, it broke its own record. In 2025, the Indo-Gangetic plains and the Nepal Tarai suffered a prolonged pre-monsoon heat wave and humidity, forcing closure of schools and workplaces. This week, <a href="https://www.dw.com/en/europe-heat-wave-intensifies-as-fresh-warnings-issued/live-73108302">southern Europe is suffering the worst heat wave</a> since temperature records began. Football matches, tennis tournaments have been affected, and tourist sites have been closed off. Qatar has ordered a midday work curfew for Nepali and other migrant workers are the maximum temperature this week touched 45°C.&nbsp; Kathmandu Valley experienced its highest temperature in 25 years in May 2024 at 35.3°C. This year, the maximum temperature exceeded 30°C on many days — heat that till a decade ago would be considered unusual. Rains in early June also meant that towns in the mountains sweltered under high heat plus humidity.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20250703090748_6975cfc2ad573f3a09ca301a299a9e92a420da7f1c5c90b8e4d061a2053dcd3e.jpg" data-media-id="editor_1" data-image-id="20250703090748_6975cfc2ad573f3a09ca301a299a9e92a420da7f1c5c90b8e4d061a2053dcd3e" data-rendition-name="original" width="1935" height="801" loading="lazy" alt="maximum average temperature in Kathmandu"> <figcaption>Source: DHM</figcaption> </figure>  Measuring just temperature does not give a true picture of how hot it is. When humidity is factored in, the heat index this summer has been much higher in northern India and Nepal. Also, the hotter the air temperature the higher the concentration of water vapour in it. “We feel it is getting hotter, and our statistics back that up,” says Shanti Kandel at the Department of Hydrology and Meteorology, which issued two heat wave warnings this year, compared to 11 last year. “We need more research to analyse how humidity is make this situation worse.” <a href="https://economictimes.indiatimes.com/news/india/india-faces-alarming-30-rise-in-moist-heat-stress-over-40-years-affecting-wide-swath-of-country-imd-study/articleshow/109376863.cms?from=mdr">A recent analysis</a> by the Indian Meteorological Department has found that heat stress in that country has increased by nearly 30% over the past 40 years. Similarly, India’s Council on Energy, Environment and Water (CEEW) noted that cities like Delhi, Chandigarh, Jaipur, and Lucknow have experienced a 6-9% rise in relative humidity in the last decade.&nbsp; It also states that <a href="https://www.reuters.com/sustainability/climate-energy/majority-indian-districts-face-high-heatwave-risk-study-shows-2025-05-20/#:~:text=%22About%2057%20per%20cent%20of,usual%20number%20of%20heatwave%20days.">60% of Indian districts</a>, home to three-quarters of the country’s 1.3 billion people face a high to very high risk from extreme heat, with rising night-time temperatures and humidity. The heat index is also called ‘<a href="https://nepalitimes.com/here-now/north-indian-heat-wave-hits-nepal">wet-bulb temperature</a>’ and is a measure of how hot the human body feels when humidity levels are also high — usually much hotter than the recorded temperature. For example, a wet-bulb temperature of 35°C is considered the maximum limit of heat and humidity that humans can handle, beyond which the body cannot cool by perspiration, leading to death. One indicator of increasing humidity is a rise in average minimum temperature, and Nepal recorded the highest figure since 1981 last year, with a peak of 15.8°C. Higher minimum temperature denotes warmer nights, which in turn is an indication of heat stress caused by increasing humidity, which in turn is a result of global warming. Aside from higher average temperatures worldwide this year, what makes heat and humidity more unbearable is that cities are always hotter than their surroundings. This is due to the <a href="https://nepalitimes.com/opinion/comment/preparing-for-kathmandu-s-heat-waves">urban heat island (UHI) effect</a> – for example the temperature inside Kathmandu’s Ring Road can be hotter by <a href="https://www.epa.gov/heatislands/what-are-heat-islands">up to 4°C during the daytime and by 1 to 3°C in the evening</a> compared to the outskirts. “Climate change is one reason for rising temperature, but there are other factors like increased heat in urban spaces due to concrete buildings and infrastructure, emissions from vehicles, industries, and home appliances,” explains urban planner Bhushan Tuladhar. He adds: “Much of this comes down to how we have developed our cities, not just our roads and buildings but also our water system, waste management, culture and customs as well as economy.” There is a feedback loop at work: as it gets hotter, more energy is used for fans, coolers, and air-conditioners which in turn add to the urban heat bubble. The way to reduce the UHI effect is to have more parks, tree-lined streets and water bodies to cool cities down.&nbsp; <a href="https://www.sciencedirect.com/science/article/abs/pii/S2212095525002093">A recent study published in the journal Urban Climate</a> by Nepali researchers at the University of Massachusetts, Tribhuvan University, University of Groningen, etc showed that even within Kathmandu, urban forests cooled neighbourhoods by as much as 1.2°C while ponds reduced the temperature by up to 0.85°C compared to nearby houses.&nbsp;  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20250703090748_e4de75dbdfb5fcfdeb0935eda364dc16b5dca8857ba335ab0f4586ebdc5093a9.jpg" data-media-id="editor_8" data-image-id="20250703090748_e4de75dbdfb5fcfdeb0935eda364dc16b5dca8857ba335ab0f4586ebdc5093a9" data-rendition-name="original" width="2580" height="1038" loading="lazy" alt="urban heat island in Kathmandu"> <figcaption>Source: URBAN CLIMATE et al.</figcaption> </figure>  ‘Our results demonstrate that blue-green spaces provide significant cooling benefits across the Kathmandu Valley, with distinct patterns by type, size, design, and urban context,’ concluded the paper, whose lead author is Saurav Bhattarai at Jackson State University in the United States. The old towns in Kathmandu Valley with traditional brick and tile architecture, ponds and trees managed hot summers better. Compact houses around a courtyard gave people just the right amount of sunlight, and use of clay mortar and bricks insulated houses in winter while cooling them in summer. There were open spaces, fertile land along the floodplains for farming, and brick pavements that allowed for seepage. “Our cities were planned taking nature into account,” says Sangeeta Singh, a professor of urban planning at the Institute of Engineering. “Kathmandu Valley is now built up, but we can still reintegrate blue-blue spaces into town planning with vertical gardening, urban forestry, using local material and harvesting rainwater.”&nbsp; Kathmandu’s municipalities have by-laws controlling building design and structure, but strict enforcement of land use and zoning are missing. Extreme heat disproportionately affects the urban poor who may not have access to fans or air-conditioners, exacerbating poverty.&nbsp; Cities in the plains have it even worse. As heat and humidity rise simultaneously, it could <a href="https://nepalitimes.com/banner/garmi-se-behal-chalo-nepal">reverse the current mass migration</a> of people from the mountains to the Tarai, where 53% of Nepal’s population lives. <a href="https://thedocs.worldbank.org/en/doc/92fbbbc6180238e18e7b239fad83e38a-0280032024/original/12-DHNT-Temperature-poverty-inequality-September-2024.pdf">A World Bank study</a> put the cost of a 1°C rise in temperature at 17.1% increase in poverty globally. Estimates put the total number of urban poor in developing countries exposed to the worst heat extremes at 26 million presently, this number is bound to grow to 215 million by mid-century, an over eight-fold increase. Meanwhile, 489,000 health-related deaths occur each year, 45% of them in Asia alone. “Heat has to be seen from a class perspective,” says Singh. “Those with money can afford gadgets and appliances to keep their homes and offices cool, but not day labourers or poor families living in cramped housing with poor ventilation.” Climate breakdown is going to widen the class divide in cities, as <a href="https://nepalitimes.com/banner/unthinkable-in-the-current-climate">summers become unliveable</a>. Says Singh: “We need policy intervention to address this class injustice. Our building by-laws and new town development must urgently integrate climate and energy efficiency elements.”

In the heat of the moment

The debate about who is less accountable to the public: politicians or bureaucrats is as old as Nepal’s democracy itself.
Some blame politicians for being beholden to the businessmen who finance their electoral campaigns, and are forced to return the favour with contracts and kickbacks when in power.&nbsp;
Others say it is civil servants who are neither civil nor servants, and know the inner workings of the system to exploit loopholes – they then teach ministers, MPs, mayors, or ward chairs which juicy projects can be squeezed. And everyone gets their share.
In reality, it is probably not a case of either, or. Both have their hands deep in the honey pot. Corruption is now such a given that yet another exposé in the mainstream press, like the latest visit-visa scam, does not raise eyebrows anymore.
We may have to edit Lord Acton’s famous quote to say that in Nepal we do not even need absolute power to corrupt absolutely. The ruling cartel has divvied up the spoils, so that no one ever faces charges. The three parties all know about the skeletons rattling in each other’s closets, and they cancel each other out.
Politicians and bureaucrats get all the blame for taking bribes, but what of the givers of bribes? In this crony capitalism, businesses invariably need political patrons in an elaborate <a href="https://nepalitimes.com/here-now/nepals-only-growth-industry-private-sector-corruption" target="_blank">national network of give-and-take</a>.
<a href="https://nepalitimes.com/here-now/nepals-only-growth-industry-private-sector-corruption" target="_blank">Politicians and businesses work hand-in-glove</a> so that conflict of interest in contracts, insider trading, cartelling, and non-performing assets of banks become the norm. Our survey after the 2017 local election showed that out of the 753 newly-elected local government chairs, <a href="https://nepalitimes.com/news/elected-contractors" target="_blank">nearly 300 were contractors</a> involved in sand-mining, quarrying, or transportation syndicates.
Nepal’s tycoons have discovered that instead of donating to election war chests of politicians, it is a much surer return on investment to spend the money to <a href="https://nepalitimes.com/news/the-business-of-politics-in-nepal" target="_blank">become legislators and politicians themselves</a>.
In democracies, there are checks and balances to control corruption when it becomes endemic. The Nepal Police and Central Bureau of Investigation (CBI) are supposed to do the detective work without political interference. The courts are required to be independent in dispensing justice and punishing crooks.
But the less said about the judiciary the better. A writ petition in the Supreme Court last week accused our sister magazine <a href="https://www.himalkhabar.com/" target="_blank">HimalKhabar</a> of contempt of court for two stories: one about how high courts have been overturning a majority of verdicts of district courts in cases of rape, and another about the Biratnagar High Court clearing a self-proclaimed holy man, Krishna Bahadur Giri, of rape despite police presenting physical evidence.
The doctrine of the separation of powers stipulates that it is when the other three pillars in a democracy are compromised that the role of the free press becomes even more vital. The world over, as soon as populist autocrats are elected to the executive, their first order of business is to co-opt the legislature and the judiciary. Then they buy off, intimidate, or neutralise the media with Strategic Lawsuits Against Public Participation (SLAPP).
Nepal’s officialdom seems to be taking midnight Zoom lessons from other despots on how to gag the media. Last month, popular talk show host Dil Bhushan Pathak was served an arrest warrant by the Kathmandu District Court for <a href="https://www.youtube.com/watch?v=-CntsnTrtG8" target="_blank">a YouTube explainer</a> about the alleged involvement of the son of Foreign Minister Arzu Deuba Rana in a reported purchase of Kathmandu’s Hilton Hotel.
The Lalitpur District Court ruled that Pathak could not be arrested without fair trial, but this week the Kathmandu District Court filed another case against the journalist based on a complaint by the Cyber Bureau, and put him on a fugitive list.&nbsp;
Without going into the veracity of Pathak’s explainer, it is deeply problematic that the Electronic Transaction Act has been invoked – proof that politicians are getting the courts and investigating agencies to make an example of a high profile journalist.&nbsp;
The intention is to silence media investigations into the fake refugee scandal in which the main partner in the ruling coalition is implicated, and in which one of its former home ministers was jailed last year.
The Kathmandu High Court has been mysteriously active in targeting journalists these days. <a href="https://bizmandu.com/" target="_blank">Bizmandu</a> and <a href="https://nepalkhabar.com/" target="_blank">Nepalkhabar</a> were served a notice last month <a href="https://nepalitimes.com/news/no-freedom-after-expression-y4inku06" target="_blank">to withdraw a story they did</a> on the Chair of the <a href="https://www.sebon.gov.np/" target="_blank">Security and Exchange Board of Nepal (SEBON</a>) Santosh Narayan Shrestha allegedly demanding kickbacks from hydropower investors.&nbsp;
Incredibly, the court even asked the two portals not to report on the subject anymore – a ruling so absurd that the Patan High Court overturned it a week later.&nbsp;
The allegations against Shrestha were made in a public meeting of the <a href="https://www.ippan.org.np/members/3060/bungal-hydro-ltd" target="_blank">Independent Power Producers Association of Nepal (IPPAN)</a>, and MPs demanded a <a href="https://myrepublica.nagariknetwork.com/news/parliament-demands-probe-into-sebon-chairman-over-alleged-commission-demand-40-32.html" target="_blank">Parliament inquiry</a> into the regulator. <a href="https://www.himalkhabar.com/144523/santosh-narayan-shrestha" target="_blank">HimalKhabar</a> reported this week that while Shrestha was reportedly demanding commissions from private investors for IPOs, he cleared primary share sales in Bajhang’s 10.75MW <a href="https://www.ippan.org.np/members/3060/bungal-hydro-ltd" target="_blank">Bungal Hydro</a> in which his family members have investments, company records show.
And then just on Monday, bureaucrats hoodwinked MPs by deleting references in a bill requiring a two-year ‘cooling off’ period under which retiring civil servants could be barred from holding constitutional positions for two years.
The contest for who is more corrupt: bureauacrats, politicians, or the private sector is on.
Kunda Dixit

kanchenjunga-glacier

Meltpools in the Himalaya

Rasuwa flood likely a GLOF

Kangchenjunga: too sacred to climb?

In the heat of the moment

SLAPPing Democracy