· &nbsp;At least 400 people are dead or missing after heavy rainfall lashed arid regions of northwestern Pakistan. Walls of mud and boulders engulfed entire villages in Khyber Pakhtunkhwa Province. More than 700 people have been killed in floods in Pakistan since June.&nbsp; · &nbsp;Over in India’s Jammu and Kashmir at the same time, multiple slurry floods on 17-18 August killed more than 80 people · A mudslide possibly caused by a glacial collapse upstream in Uttarakhand on 5 August nearly wiped the village of Dharali off the map. At least 70 people, 23 of them Nepalis are dead or missing. · On the night of 8 July, <a href="https://nepalitimes.com/news/rasuwa-flood-likely-a-glof">glacial lakes in Tibet overflowed</a>. By dawn the mudflow had demolished the Nepal-China border bridge killing at least 11 people, destroyed hydropower plants, swept away bridges, roads, over 100 cargo trucks and newly imported electric vehicles. All these disasters have a common thread: a cascade of hazards caused by record-breaking rainfall on fragile Himalayan slopes destabilised by melting glaciers and permafrost, seismicity and poorly engineered infrastructure. They are called ‘rain bombs’ — a heavy localised downpour measuring more than 100mm/h on a steep mountainside. As global warming heats the atmosphere, warmer air can hold more water vapour. The heavy rain then falls where there should be snowfall: on moraines and slopes that have lost the permafrost adhesive that held the debris together. “Increasingly, there is now more rainfall at higher altitudes where there used to be snowfall previously, and this directly impacts loose material in that fragile landscape which moves down,” explains Mohan B Chand, a Himalayan Glaciologist at Kathmandu University. “Moreover, the rains these days are heavy and fall within a few hours. So even a small burst has bigger impact.” The <a href="https://nepalitimes.com/banner/drones-to-the-rescue-in-melamchi">2021 Melamchi flood</a> and the <a href="https://nepalitimes.com/news/sikkim-flood-is-warning-to-nepal">Sikkim disaster in 2023</a> have been attributed to record-breaking torrential rain on a glacial moraine that collapsed, unleashing a catastrophic debris flow.&nbsp; The Bhote Kosi flood this year happened even without torrential rain, and originated at rapidly expanding supraglacial lakes that overflowed, similar to what happened on the Mendenhall Galcier in Alaska last week. In Uttarakhand, the trigger could be in the upper catchment cryosphere, or a landslide dammed lake. Basanta Raj Adhikari of the Centre for Disaster Studies at the Institute of Engineering also calls them ‘sediment bombs’. He clarifies: “There is lots of sediment up there from landslides or glacial activity, and when there is heavy rainfall and hotter temperature, they are unleashed downstream. One thing is for sure, these extreme events are getting more frequent and more destructive.” Researcher Alton C Byers who has studied melting glaciers in the Himalaya and Andes names the eight most potentially dangerous glacial lakes in Nepal: Lower Barun, Chamlang North Tso, Chamlang South Tso, Dig Tso which burst in 1984, Lumding Tso, Thulagi, Tso Rolpa and Imja Tso (see map).  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20250822030844_70b3bf6a1ad9b9f9481c9af860629b2a05ac1338a3b89a831506f1c6bdddf5ec.jpg" data-media-id="editor_3" data-image-id="20250822030844_70b3bf6a1ad9b9f9481c9af860629b2a05ac1338a3b89a831506f1c6bdddf5ec" data-rendition-name="original" width="522" height="557" loading="lazy" alt="high risk glacial lakes in Nepal"> </figure>  Of these, Tso Rolpa and Imja have been lowered by 3m each, while Thulagi, Lower Barun, Lumding Tsho, and Hongu 2 glacial lakes have been targeted for lowering by the Department of Hydrology and Meteorology as part of the recent Green Climate Fund grant of <a href="https://nepalitimes.com/here-now/meltpools-in-the-himalaya" target="_blank">$36.1 million awarded to Nepal</a>. “These lakes have changed over the years as their debris-covered glaciers continue to recede,” Byers told Nepali Times. “When water volume in the lake basin increases, they become more vulnerable to flood triggers such as overhanging ice as glaciers recede further to their headwalls, and permafrost on their moraines continues to melt.” <h2>These are not ‘natural disasters’</h2> Scientists have given the current planetary epoch a name: the Anthropocene. And anthropogenic causes in this era heighten the risk of disasters. Indeed, an analysis of recent Himalayan calamities (page 1) shows that there is much more at play here than climate breakdown. Haphazard encroachment of floodplains, quarrying and crusher activity exacerbated the effect of <a href="https://nepalitimes.com/editorial/when-it-rains-it-pours-ksqprbu3">extreme rainfall on 28 September around Kathmandu Valley</a> that killed 200 people. The human cost of the 5 August catastrophe in Uttarakhand would have been high in any case, but the fact that the tiny village had expanded across a vulnerable alluvial fan to cater to a tourism boom meant more death and destruction. There are similar alluvial fans across Nepal, where small towns have expanded because new highways follow rivers, like Beni located at the confluence of the Myagdi Khola and Kali Gandaki. Other towns like Kagbeni or Damauli are located on the banks of rivers and tributaries that are directly downstream from rapidly expanding glacial lakes or unstable mountains. “In Butwal, people are building houses on the floodplain of the Tinau River, and yet people blame climate change or rainfall when there is a disaster,” says Basanta Raj Adhikari at the Institute of Engineering. “This is happening all over the country. Imagine the kind of devastation Beni would suffer if there was a big flood.”  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20250822030848_ed411f8618c7a411ed4c165e91f3b880abb085a8a511405710dd8220f657da84.jpg" data-media-id="editor_6" data-image-id="20250822030848_ed411f8618c7a411ed4c165e91f3b880abb085a8a511405710dd8220f657da84" data-rendition-name="original" width="1200" height="800" loading="lazy" alt="Beni Bazar"> <figcaption>RISKY CONFLUENCE: Beni has expanded rapidly after the highway to Mustang was built. But the town is situated on the alluvial fan of past flash floods on both the Kali Gandaki and Myagdi Khola which have dangerous glacial lakes in their upper catchment. Photo: BENI TOURISM</figcaption> </figure>  Traditionally, Nepal’s villages and settlements were located high above rivers because our forebears learnt lessons from recurring flash floods. Now, the road network follows rivers, and towns have sprung up along these highways. Even when roads are not on river banks, many gouge out slopes above, unleashing massive landslides that block rivers. Experts say Nepal’s hazard map should now be updated for glacial outbursts so municipalities can plan risk-sensitive land use zoning. This &nbsp;must go hand-in-hand with measures to reduce the risk by structural mitigation, such as engineering and construction, and then with risk awareness and early-warning systems. Says Himalayan researcher Alton C Byers: “Sooner or later, communities will realise that certain sites are simply no longer safe for a village or city, especially because of climate change in the mountains. The Himalaya has always been high-risk with its steep slopes, thin soil, monsoon rainfall regime, and frequent seismic activity. So, some places are no longer safe to live in.” Mohan B Chand of Kathmandu University adds that <a href="https://nepalitimes.com/banner/climate-smarter-himalayan-infrastructure">hazard mapping is especially crucial for expensive hydropower plants</a>: “Most of these are on snow-fed rivers, but environmental risk assessment is not taken seriously.” He says that because Nepal is set to generate 28,500MW by 2035 to meet its carbon neutral target, the government must work to minimise upstream risk by integrating disaster mitigation components in new energy investments. Few know that Nepal’s first hazard mapping was done 40 years ago in the Khumbu with a United Nations University study titled ‘Highland Lowland Interactive Systems’. It is hard to find that document anywhere. Today, hazard mapping technologies, satellite remote sensing, drones, synthetic aperture radar (SAR) and modelling with AI have made it much easier to integrate multi-hazard risk assessment. That data needs to be made available to local governments so they can plan. Cell phones and new apps that monitor real-time glacial lake levels, live precipitation and hydrological data, and local weather forecasts can make early warning systems more effective. Recent disasters have shown that even the smallest of glacial lakes that are rarely considered in risk assessments can cause much damage. Langmale Lake in the Barun Valley was less than 0.1 km2 in size, but <a href="https://nepalitimes.com/here-now/nepal-s-mountains-are-melting" target="_blank">the flood in 2017</a> caused extensive downstream damage. The 2012 Seti flood in Pokhara, the Chamoli disaster in Uttarakhand in 2021, the South Lhonak proglacial lake burst in Sikkim in 2023 that washed away the $1.7 billion Chungthang Teesta III Project, and the August 2024 floods above Thame in Khumbu are other recent examples.&nbsp; Byers thinks some of these floods may have been initially triggered by massive rockfall or moraine collapse related to <a href="https://nepalitimes.com/multimedia/the-not-so-permanent-frost" target="_blank">melting permafrost</a>. The size of a glacial lake alone does not determine the severity of destruction. What makes all the difference is downstream development, and if there pre-warning. Dig Tso in Khumbu which burst in 1984, was much larger than the lake that caused the Bhote Kosi flood in July, but the economic cost to the country of the trans-boundary disaster this year was much higher. Says glaciologist Chand: “We have to monitor the lakes, not just via remote sensing but with field visits. These may be costly, but mitigating the risk is less expensive than the disasters themselves.” Nepal has the technology and trained personnel to do hazard mapping, monitoring, and to design early warning apps. That data and information now needs to be available to all three levels of government to improve preparedness and risk reduction. “The cascading and compounding hazards are increasing in the Himalaya, this must be the subject of our research now,” says Adhikari at the Centre for Disaster Studies. “Recent events are a wake-up call, if we do not take this seriously things may be more dangerous in future.”

Sonia Awale

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Rain bombs

<a href="https://nepalitimes.com/banner/including-local-knowledge-to-study-climate-change">Alton Byers</a> has organised frequent research expeditions to the Himalaya for more than 50 years. Recently, he returned to the <a href="https://nepalitimes.com/banner/tracing-past-glacial-floods-in-kangchenjunga">Kanchenjunga region</a> which he has visited three times since 2019. His team was there to gather more data for an ongoing study of glacial, ecological and socioeconomic changes in the region. But, his attention was soon diverted when a young man from the local community told Byers that locals had noticed large meltwater ponds forming at the toe of the <a href="https://nepalitimes.com/here-now/saving-kangchenjunga">Kanchenjunga</a> Glacier, upstream from Ghunsa and Kambachen. “He asked if we could go take a look at it,” Byers said. “We were on our way up to the Kanchenjunga base camp, so we made a detour. Sure enough, you could see these considerable lakes, perhaps a half-a-square-mile and growing.” Byers sprung into action. First, he interviewed other community members about the ponds — they confirmed the observations and growing concern. Then, over the ensuing months, he assembled a team of experts to conduct a study of how the ponds were changing. <a href="https://www.mdpi.com/2073-4441/17/10/1457#:~:text=This%20study's%20modeling%20results%20suggest,Ghunsa%20in%20the%20form%20of">The study was published in the journal Water earlier this month</a>. The paper outlines a number of potentially dangerous flood scenarios that could be triggered at the site in the future. The researchers urge regional authorities to implement mitigation measures, including a monitoring program and an early warning system for flooding.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20250708030756_e4eda873993e7aa17a2e90dc95a162c85e4dc4627f6251ee8a9543681e3367b3.png" data-media-id="editor_4" data-image-id="20250708030756_e4eda873993e7aa17a2e90dc95a162c85e4dc4627f6251ee8a9543681e3367b3" data-rendition-name="original" width="1967" height="2128" loading="lazy" alt="Mapping Kangchenjunga glacial flood risk"> <figcaption>Predicted future Kanchenjunga proglacial lake extent and depth, frontal moraine, and potential avalanche location, which were used as input for modeling the GLOF cascade in r.avaflow. The background image is from Google Earth Imagery taken on 25 December 2020.</figcaption> </figure>  Byers’ first call for collaboration was to <a href="ttps://www.icimod.org/team/sonam-wangchuk/">Sonam Wangchuk</a>, an expert in snow and ice research via satellite imagery at the International Centre for Integrated Mountain Development. The images were striking. From 2022 to 2024, the ponds grew from puddles to large, interconnected bodies of water.&nbsp;  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20250708030740_d60cec33fe26074cb49a6a7c4d8f42ef8870c63f606c945d60fc3bf0327b1a3b.png" data-media-id="editor_6" data-image-id="20250708030740_d60cec33fe26074cb49a6a7c4d8f42ef8870c63f606c945d60fc3bf0327b1a3b" data-rendition-name="original" width="1861" height="2126" loading="lazy" alt="Mapping Kangchenjunga glacial flood risk"> <figcaption>Evolution of supraglacial lakes on debris-covered glacier (27.7726, 88.0187) at Kanchenjunga. Time series satellite composite images were acquired by Sentinel-2 Multispectral Instrument between September and October, with the exception of the April–May 2024 images. Two large and distinct lakes which expanded rapidly in 2022 and continued to grow in 2023 and 2024 are labeled as 1 and 2, for locational comparison with the oblique view taken on 25 May 2024. Photo: ALTON BYERS</figcaption> </figure>  “It’s sort of an indicator of how these melting processes are accelerating,” Byers said. Next, Byers and collaborators estimated that the meltwater ponds could form a large glacial lake. That lake, if it forms, will be vulnerable to <a href="https://nepalitimes.com/here-now/nepal-s-mountains-are-melting">outburst flooding</a>, which could be triggered by melting processes, structural collapse or rockfall from surrounding slopes. Finally, the researchers focused their efforts on modeling potential floods. They identified four scenarios, from small to large.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20250708030744_ecafcf2013548954fcd0c76ce9ab299d68222fae99892d168dcba70f0fd802ae.png" data-media-id="editor_8" data-image-id="20250708030744_ecafcf2013548954fcd0c76ce9ab299d68222fae99892d168dcba70f0fd802ae" data-rendition-name="original" width="2637" height="3197" loading="lazy" alt="Mapping Kangchenjunga glacial flood risk"> <figcaption>Flood extent under various scenarios: areas impacted by all four GLOF scenarios are labelled as 4, those affected by three scenarios as 3, by two scenarios as 2, and by only one scenario as 1. (B) Hydrograph generated from GLOF modeling in r.avaflow and used as the input flow data for modeling each GLOF scenario in HEC-RAS. Flow depth and velocity at Kampachen (C,D) and Ghunsa (E,F). Discharge rate and time of peak, and flow arrival at Kampachen (G) and Ghunsa (H) under different scenarios.</figcaption> </figure>  Under the mildest scenario, the flood surge would travel 100km down the Tamor River, and under the worst-case scenario it would travel at least 220km with impact on houses and bridges, livestock, crops and tourism infrastructure. Byers warns that without adequate preparation, glacial outburst flooding can be deadly. The paper advises local and regional authorities to take measures to prevent a flood originating from the study site. Their recommendations include establishing early warning systems for flooding, partnering with research organisations in Kathmandu to monitor the site and adapting zoning laws to prevent new buildings in flood zones.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20250708030748_dccee85332d2844413dc5693050899b4bc49a25f9c66abc6b1ac1f5a80786d58.jpg" data-media-id="editor_9" data-image-id="20250708030748_dccee85332d2844413dc5693050899b4bc49a25f9c66abc6b1ac1f5a80786d58" data-rendition-name="original" width="1356" height="668" loading="lazy" alt="Mapping Kangchenjunga glacial flood risk"> <figcaption>Imja Lake, a glacial lake in the Mount Everest region of Nepal, began as meltwater ponds in 1962 and now contains 90 million cubic meters of water. Its water level was lowered to protect downstream communities. Photo: ALTON BYERS</figcaption> </figure>  Read also: <a href="https://nepalitimes.com/multimedia/the-not-so-permanent-frost">The not-so-permanent frost</a>, Wilfried Haeberli and C Alton Byers One of the cheapest and most effective early warning systems is deceptively simple: cell phones. Says Byers: “Not everyone can afford multi-million dollar early warning systems that rely on laser readings of water depth. But, studies have shown that cell phones, at least during the daytime, are one of the better early warning systems out there.” Byers hopes the study can help the same people that brought the issue to his attention: “The goal was always to share the research with the local community. Then they have all of the information they need to make the best decisions possible.” <a href="https://www.colorado.edu/instaar/2025/05/27/researchers-model-dangerous-glacial-lake-himalayas-and-propose-solutions">Gabe Allen</a> is Senior communications specialist at the Institute of Arctic and Alpine Research at the University of Colorado Boulder.

Mapping Kangchenjunga glacial flood risk

<a href="https://nepalitimes.com/banner/human-face-of-a-himalayan-climate-crisis" target="_blank">Janmu Sherpa</a> was a grandmother with a dozen goats and a tea house in Donggang in the Rolwaling Valley. Her stopover served trekkers en route to Tso Rolpa Glacial Lake and the trail over Tashi Laptsa Pass to Khumbu. In 2018, I spent months in the Rolwaling Valley studying how <a href="https://www.ted.com/talks/rastraraj_bhandari_what_climate_activists_are_doing_wrong" target="_blank">mountain communities perceive</a> climate change. Unlike my climate-anxious self, Janmu was calm, even hopeful, despite having lived through floods, landslides, and the 2015 earthquakes. “No one knows when Tso Rolpa will burst, so we cannot stop our daily chores. Let fate decide,” Janmu Sherpa had said. Last year, fate did decide. On 22 June 2024, the Dorji Phungmo Glacial Lake burst. The resulting flood swept through the Rolwaling River, washing away homes and hotels in Donggang. Janmu <a href="https://thehimalayantimes.com/nepal/climbers-valley-devastated-by-floods-immediate-relief-sought" target="_blank">was among</a> the missing, and later declared dead.&nbsp; I learned of her disappearance during a recent cycling trip through Panauti along the <a href="https://nepalitimes.com/multimedia/a-flood-of-tears-on-the-rosi" target="_blank">Rosi Khola</a>, which was devastated by deadly flash floods on 28 September 2024.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/2025051918054_14898953b7a5808b51440f7a6fa35a7d66146bbb1d62bf88729a83a558ca8ebf.jpg" data-media-id="editor_4" data-image-id="2025051918054_14898953b7a5808b51440f7a6fa35a7d66146bbb1d62bf88729a83a558ca8ebf" data-rendition-name="original" width="1500" height="1000" loading="lazy" alt="A pre-monsoon déjà vu"> <figcaption>Tso Rolpa glacial lake at 4,580m has grown seven times in size in the past 60 years due to global warming. </figcaption> </figure>  Tipper trucks rumbled through the dusty road, carrying stones and gravel from unregulated quarries and sand mining along the Rosi. This was destruction disguised as development, and the crusher industries had <a href="https://nepalitimes.com/news/the-revenge-of-the-rivers" target="_blank">magnified the impact of record rainfall</a>. On the other side of the mountain, along the Lele and Karmanasa Khola, families are still reeling from last year’s floods. Here, too, a quarrying frenzy exacerbated the <a href="https://nepalitimes.com/banner/nepal-valley-suffers-quadruple-disaster">destructive power of the floods</a>. There are thousands of untold stories like Janmu, and the estimated 200 who perished in the September floods. Most have been forgotten, their deaths blamed on fate. I write this from afar, as Kathmandu hosts the Sagarmatha Sambaad this week to draw global attention to the impact of the climate crisis on the Himalaya. The summit took place as pre-monsoon rains lashed the Rosi and Lele Valleys. Even before the start of the rainy season, more debris flows from the mining operations destroyed repaired roads and neighbourhoods rebuilt after floods last year. The rivers that flooded Kathmandu in September 2024 are still vulnerable. Aside from a few sandbanks built by local hands, nothing has changed. No national reckoning. No systemic response. Instead, everything is blamed on climate change.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/2025051918054_57fa57586b1e370e715daf837aa4cae3e73b0f029bb0ccef8be768e85656cc5f.jpg" data-media-id="editor_7" data-image-id="2025051918054_57fa57586b1e370e715daf837aa4cae3e73b0f029bb0ccef8be768e85656cc5f" data-rendition-name="original" width="1499" height="1000" loading="lazy" alt="A pre-monsoon déjà vu NT"> <figcaption>Janmu Sherpa's village of Donggang is directly downstream from Tso Rolpa Glacial Lake.</figcaption> </figure>  <a href="http://as%20kathmandu%20hosts%20the%20sagarmatha%20sambaad/" target="_blank">Janmu Sherpa’s story</a> haunts me not just because of her loss, but because she shaped my journey as a climate activist. She taught me that climate action is not just about carbon or conferences, it is about livelihoods, listening, and the impossible trade-offs faced by communities where survival is more urgent than sustainability. As monsoon clouds gather again, there is a sense of dread not just about floods, but for the apathy that follows. We are trapped in a cycle of climate inaction fueled by corruption, state neglect, and a development model that treats rivers as resources to be drained, not lifelines to be protected. It is no longer a question of if the floods will come, but when, and how devastating they will be. And yet, <a href="https://nepalitimes.com/here-now/politicians-and-cronies-blamed-for-kavre-floods" target="_blank">those in power remain unmoved</a> even when disaster strikes their own backyard. We are still chasing climate finance and hosting international summits, while local insurance markets stagnate and communities fend for themselves. To be sure, global advocacy matters. The Himalayan climate crisis must be on the international agenda. Melting glaciers here affect billions downstream. But adaptation cannot begin and end in air-conditioned conference halls. It must bring real preparedness to villages, valleys, and riverbanks of Nepal.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/2025051918058_3ec77114d434385351ad1637fd5ab42dc6a76b94b0e90f1c6e683c71535f6e6a.jpg" data-media-id="editor_10" data-image-id="2025051918058_3ec77114d434385351ad1637fd5ab42dc6a76b94b0e90f1c6e683c71535f6e6a" data-rendition-name="original" width="1701" height="1000" loading="lazy" alt="A pre-monsoon déjà vu"> <figcaption>The Sagarmatha Sambaad climate conference in Kathmandu this week. Photo: PRADEEP RAJ ONTA / RSSseasonmedia2007</figcaption> </figure>  I visited the communities ravaged by floods in September and as I wrote in <a href="https://nepalitimes.com/opinion/flood-of-despair" target="_blank">Nepali Times</a> then, top-down responses are always too little, too late and too ineffective. The only real solution is bottom-up, community-led adaptation. Those who lived through the floods know what needs to be done, and those privileged and in power need to enable them. Community-led adaptation is not just a buzzword. It is our only viable path forward. It means empowering local people with the tools, knowledge, and resources to protect themselves. It means investing in early warning systems that reach the last mile and actually work, restoring ecosystems that buffer floods, and supporting indigenous knowledge that has long helped communities live in harmony with nature. It means letting go of our belief that somehow our degrees in climate change and attendance in global climate conferences enable us to tell communities how they should be responding to climate change. It means shifting power and funding to the grassroots, where resilience is not theoretical — it is lived, practiced, and urgently needed. As the rains return, I am reminded of Janmu Sherpa’s voice of quiet wisdom. Her innate resilience did not save her life. Let us not wait for the next flood to act. Let us protect what we still have. Rastra Raj Bhandari is co-founder and fellow at the Himalayan Water Project, where he leads the research on climate finance opportunities for the Himalaya.

A pre-monsoon déjà vu

In the first two episodes of this series, we looked at how <a href="https://nepalitimes.com/here-now/people-and-mountains-are-thirsty-in-eastern-nepal">climate breakdown has worsened the water shortage in eastern Nepal</a>, with rains failing and springs going dry.&nbsp; But there is a flipside. In the monsoon, there is also the curse of too much rain leading to destructive landslides, floods driving people out.&nbsp; <a href="https://nepalitimes.com/here-now/climate-crisis-drought-food-deficit-migration">Analysing meteorological and hydrological data from the past half-a-century in eastern Nepal’s Tamor River basin</a>, the big floods of 1963 and 1968 stand out with other less destructive monsoons in between.&nbsp; Nepal’s monsoons usually last 112 days from mid-June to mid-September, and its clockwork arrival and departure has inspired Nepali poetry and song. But climate breakdown has disrupted the timetable, and there have been years with highly unusual monsoons and floods. In 1968, the monsoon delivered more rain than usual in some places and less than normal in others, and the big floods actually came after the monsoon is supposed to have retreated.&nbsp; The national news agency RSS reported a damaging flood in Sunsari, the district in the plains where the Kosi River disgorges into the plains after confluence of the Arun, Sun Kosi and Tamor. Three days later, RSS reported that 500 cattle and 1,500 goats had drowned in Sunsari, and a child’s body had been found. And upstream in Leuti Khola, three people and seven houses were swept away. A week later, RSS reported again that seven people and 14 livestock had been killed by floods, and bridges as well as paddy ready for harvest were swept away. Even upstream in Olangchung Gola, three people were killed.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20240427010452_9fe3ea424cd644cb1f5a06a731f44d466d70216f39d943e0bd4a5f6f13fdf90d.jpg" data-media-id="editor_2" data-image-id="20240427010452_9fe3ea424cd644cb1f5a06a731f44d466d70216f39d943e0bd4a5f6f13fdf90d" data-rendition-name="original" width="1688" height="1088" loading="lazy" alt="Water crisis in Eastern Nepal"> </figure>  Laxmi Prasad Siwakoti was a boy in 1968, and remembers enormous boulders thundering down rivers. One boulder the size of a house luckily was pushed to the banks before it could destroy a key bridge below Taplejung. All this water created even more death and destruction in the inland delta of Sunsari, also washing down the bodies of people and livestock from upstream. The 1968 post-monsoon flow of the Kosi reached 23,106 cumecs – four times the volume in the 1963 flood. Some researchers attributed the 1963 flood to the bursting of Tiptala Glacial Lake in the Kangchenjunga area, and that the 1968 flood was also caused by another moraine collapse on the same lake.&nbsp; But analysis of precipitation data of the Department of Hydrology and Meteorology shows that the reason for the catastrophic floods of 1968 was unusually heavy post-monsoon rainfall in the Tamor basin. Archival records of rainfall at Mulghat below Dhankuta shows that there was 162mm of rain on 3 October and another 158mm on 4 October. This meant that one-third of the total rainfall during four monsoon months fell in just two days. Never had Mulghat recorded so much rain in such a short time, and in the 55 years since there has been that much rain only twice. On 4-5 October 1968, Dhankuta received 300mm of rain. It had never received so much rain in the autumn before or since. Similarly, Taplejung recorded 231mm of rain in the same two days – it has never received so much rain in the post-monsoon since. Hydro-meteorological stations across eastern Nepal in Panchthar, Taplejung, Dhankuta and Sankhusabha all show data of record-breaking post-monsoon precipitation on 3-4 October 1968. In fact data shows that except for northwestern Nepal, there was heavy unseasonal rain all over. Dhulikhel near Kathmandu recorded 221mm rain that day, and even Jomsom in the trans-Himalayan rainshadow got 58% of its annual rainfall in just one week. In a paper titled Heavy Monsoon Rainfall in Nepal, J L Nayava dug up an archival weather map from 1968 that showed a cyclone develop in the Bay of Bengal a week after the official retreat of the monsoon from Nepal in conjunction with a low pressure area over southern India. Both systems moved northwards, and it could have been the combination of the two that dumped the record rainfall in Nepal.&nbsp; Nayava notes: ‘On 29 September, a small low appeared over the Bay of Bengal at about 10°N, 90°E. During the next two days, the circulation of this low expanded as it moved north-eastwards into central India and intensified into a depression. By 3 October, Nepal and much of India had come within the circulation of this depression… During the next two days, a sharp 500mb trough passed through Nepal and central India and as the polar westerlies at 200mb intensified and moved equatorwards, bringing the subtropical westerly jetstreams ever closer to Nepal. As the depression moved north, the anticyclonic circulation at 200mb over the depression intensified and became orientated in a south-west-north-east direction. Associated with these developments, widespread rain fell in most parts of Nepal…’  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20240427010452_6fc01e56307dfd3c43e58d7170346d11a1fd8ee2a748074b22aa84bcfdab8369.jpg" data-media-id="editor_3" data-image-id="20240427010452_6fc01e56307dfd3c43e58d7170346d11a1fd8ee2a748074b22aa84bcfdab8369" data-rendition-name="original" width="1500" height="1000" loading="lazy" alt="Water crisis in Eastern Nepal"> </figure>  It was not just eastern Nepal that suffered destruction, many people were killed in Bhojpur, Khotang and Solu to the west. If this was indeed a glacial lake outburst flood, the destruction would not have been so widespread. The hydrological data of the Tamor of 3-5 October 1968 are also not commensurate with a flash flood triggered by a glacial lake burst. The Mulghat hydrological stations showed that on 4 October, there was 3,060 cumec of flow (volume of water never recorded before) which decreased only slightly over the next few days and returned to a more normal 636 cumecs only on 9 October.&nbsp; By the time the rains stopped that October, 60 people were dead in Kosi zone alone, thousands of livestock were killed and houses swept away. The new bridge over the Tamor and other suspension bridges were destroyed. But that was not the end of the story. On 29 October 1968 came news that 91 people had been killed in Taplejung, 60 in Terathum, 30 in Panchthar and three in Dhankuta. Just in the Tamor watershed, 184 people were killed and thousands made homeless. Nepalis have learnt over the years to be prepared for disasters during the monsoon, and to breathe a sigh of relief when the rains end. But the 1968 floods hit after the monsoon, when people felt safer. Floods were nothing new in the Tamor. There was an unimaginable one five years earlier on 15 August 1963 that swept away 16 houses in Olangchung Gola, and this flood was different from the one in 1968. Locals remember an air blast preceding the flash flood, and an approaching roar that shook the mountains like an earthquake. Houses shook, cattle cowered and goats ran for cover. Upstream, villagers saw clouds of dust and spray, and there was a smell of gunpowder in the air as enormous boulders collided with each other. Although this was the monsoon period, the precipitation in the day preceding the debris flow was normal. This could not have been caused by a cloudburst. Alton C Byers, the American glaciologist who has researched historical glacial floods in the Kangchenjunga region, used satellite imagery and interviews with local villagers to pinpoint the flood to the bursting of Tiptala glacial lake at 4,900m. “The gunpowder smell and the wind preceded the arrival of the debris flow,” remembers Nil Limbu of Chhiruwa of Taplejung, an eye witness of the 1963 event. “It destroyed everything, took away all the trees, left just rocks and boulders.” The flood washed away the mule trail along the Tamor, and swept away the flat meadow along the river where there used to be a weekly market. Today, the trail is higher above the river, but for years later, there used to be rockfalls from above. The debris flow raced downstream destroying houses, trails, bridges, farms, livestock. The flood made national news, and RSS reported that below Dhankuta, the Tamor destroyed the trail to Taplejung and washed away seven bridges. The glacial lake outburst flood on the Tamor met the Arun and then the Kosi where the river flow spiked to 6,371 cumecs. Further downstream in the plains, the flood destroyed the western embankment of the Kosi Barrage, inundating villages in more than 1m of water. A month later, the government released the death toll: 32 killed, unknown number of livestock, standing crops, and causing damage equivalent to 1.6% of Nepal’s annual budget that year. Nepal’s famous eye doctor Sanduk Ruit’s family also had to leave their home in Olangchung Gola after that flood and settled down in Dhankuta. The combined result of the record rainfall-induced floods of 1968 as well as the glacial lake outburst flood of 1963 could have been early examples of climate-induced floods, which have become more frequent in recent years.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20240427010456_c6e6182935c1704629e175dc351f79b74367824a14be020d0b05bdda201a2747.jpg" data-media-id="editor_4" data-image-id="20240427010456_c6e6182935c1704629e175dc351f79b74367824a14be020d0b05bdda201a2747" data-rendition-name="original" width="1036" height="1184" loading="lazy" alt="Water crisis in Eastern Nepal"> </figure>  On 17 June 2023 Memeng station in Panchthar recorded 230mm rainfall in a 24 hour period, the highest rainfall ever recorded in that station (second highest was 148mm in July 2002). Nearby Dovan of Taplejung experienced 106mm on 18 June and 102mm on 19 June. The basin-wide floods on the Tamor and its tributaries caused damage worth at least Rs8.5 billion on 30 hydropower plants in Sankhuwasabha, Taplejung and Panchthar. Eighteen workers were killed. Half of these schemes were under construction, but plants generating 130MW were knocked out of action. Some, like the Upper Piluwa Khola 2 and Super Hewa Khola have still not been repaired. While these were all caused by extreme rainfall events, on the Sikkim side of Kangchenjunga a post-monsoon disaster on 4 October 2023 washed away several hydropower plants on Teesta and its tributaries, and killed nearly 100 people downstream. The 1,200MW Chungthang Dam built at a cost of $1billion was destroyed. It was later revealed that extreme rainfall on the South Lhonak Glacial Lake, north of Kangchenjunga, caused the collapse of a lateral moraine which allowed a wave to breach the terminal moraine. The lateral moraine could have been weakened by thawing permafrost, and collapsed during heavy rainfall on the night of 4 October.&nbsp; The Sikkim disaster was an important lesson for Nepal, which has invested heavily in infrastructure on this side of the border. More than a dozen medium and large hydropower plants have been built or are under construction along the Tamor alone. The 1960 Tiptala and the 1980 Nangama glacial lake bursts are further proof that such disasters can happen again without warning because of climate breakdown. Besides droughts and floods, landslides are also the reason many people from eastern Nepal have migrated to the relative safety of the plains. A huge landslide in 1946 in Hangdeva in Taplejung is still displacing many people. East of Hangdeva, another landslide in 1977 killed 25 people and the rest of the village just moved out. It is clear that with the climate crisis, extreme weather events and glacial lake bursts will be more serious and frequent, affecting lives and livelihoods, contributing to outmigration.&nbsp; This is the final of a three-part series supported by the Barbara Foundation.

Either too little, or too much water

Nepal showed inconsistent performance at the T20 World Cup 2026 in Mumbai with flashes of brilliance, but ultimately snatched defeat from the jaws of victory. The <a href="https://nepalitimes.com/news/rhinos-hit-the-ground-running">near-win against England</a>, a test cricket team by an associate country, in the opening game showed promise and suggested that Nepal’s cricket was on the cusp of glory. The Nepal Premier League and a flawless performance in the qualifiers had raised hopes that perhaps the Rhinos could progress out of the group stage. However, subsequent losses against newcomers Italy and the West Indies were harsh reality checks about the true state of the game: there is a lot of catching up to do in the present, and structural changes to put in place to win big in the future. Head Coach Stuart Law summed it all up quite harshly: “To go from that high to then go to an extreme low four days later, that’s not showing mental toughness.” He was worried about the distraction of social media and lack of focus among players: “When you’re in cricket, do your cricket. It’s a difficult one for me because I’m a social media dinosaur, I don’t understand it. You don’t have to keep showing your face if we’re winning games.” Finally a late-night win against Scotland on Tuesday redeemed some of Nepal’s pride. A strong opening partnership, yet another rugged Dipendra Singh Airee innings and Sompal Kami’s vindictive 3 for 25 helped Nepal beat Scotland in their last group game at the T20 World Cup.  <figure><img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20260218010220_6ca369f6aefc8b653c2572467f050e96b029c96b71fed5fb4213898c7d469325.jpg" data-media-id="editor_1" data-image-id="20260218010220_6ca369f6aefc8b653c2572467f050e96b029c96b71fed5fb4213898c7d469325" data-rendition-name="original" width="1366" height="2048" loading="lazy" alt="T20 World Cup Nepal"></figure>  There was nothing riding on the game but honour, it means at least that Nepal do not crash out on zero. The game ebbed and flowed. Scotland started well and looked set to score 200 before collapsing in the end at 170. The Nepal batting effort also started out well, but in the middle overs after some wickets had fallen, it looked like the team was whimpering out again. Boundaries dried up, the run rate creeped up to almost 13, before Airee and Jha woke up and took charge and got to 171 with a few balls to spare. The dhaka topi crowd in the stands loved it. A big part of the reason Nepal’s performance was so much better against England than in the other games was the mentality going in. Against England, Nepal were clear underdogs and could play freely. Even a nasty defeat would have been forgiven. Against newcomers Italy, these roles were flipped. Fans and perhaps the players underestimated Italy, a nation much better known for its football culture. But it had put together a smart, experienced team made up of Italian cricketers with South African, Australian, English, Indian, Pakistani and Sri Lankan heritage. And Nepal may have won a series against West Indies last year, but against the full strength Caribbean squad they were easily beaten.  <figure><img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20260218010220_dc27adaa2102b493f940a97f9572769e695c2c1c41c8558fc4c23657cc1c3261.jpg" data-media-id="editor_2" data-image-id="20260218010220_dc27adaa2102b493f940a97f9572769e695c2c1c41c8558fc4c23657cc1c3261" data-rendition-name="original" width="2048" height="1366" loading="lazy" alt="T20 World Cup Nepal"></figure>  Another key difference is that Nepal was batting second against England. Against Italy and the West Indies, having to set a target rather than chase it, there was miserable batting failure. The front of the order — openers Kushal Bhurtel and Aasif Sheikh, captain Rohit Poudel — did not pace themselves well. They started much too slow, not able to take advantage of the first six powerplay overs. Airee’s 58 and Sompal Kami’s 26 off 11 against the West Indies were the only innings of any note. The middle order of Bam, Jha, Aarif Sheikh was not much better. Nepal really struggled with the ball too in that game, taking the one wicket against the West Indies and none against Italy. Of course, it is a huge ask of your bowling attack to defend anything below 150 in the modern T20 game. There were questionable tactical choices. Early wickets are essential when defending a low score. But key wicket taker Sandeep Lamichhane was not brought on until the middle overs, when the opponents had made too many runs to feel any fear. So they took him on and he had a really poor tournament, going for a lot of runs.  <figure><img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20260218010220_b0301b854ddf235e1bcb84e8ed58060a68c8f3f13d3bb5a7596e1f51184e0d03.jpg" data-media-id="editor_3" data-image-id="20260218010220_b0301b854ddf235e1bcb84e8ed58060a68c8f3f13d3bb5a7596e1f51184e0d03" data-rendition-name="original" width="1366" height="2048" loading="lazy" alt="T20 World Cup Nepal"></figure>  To captain Poudel’s credit, he acknowledged the bad showing against Italy: “It was not a 123 all-out wicket. We are professionals and not turning up for the game was disappointing.” Coach Law thinks that Nepal is going to get to the next step. If the team is ambitious, and hopes to compete at the elite level, then it cannot celebrate a loss against England. If it wants to win consistently, it has to shed the ‘Cardiac Kids’ nickname. It is better to win than to be fun to watch but lose. The T20 game is so brisk and so it is often won in the margins. Good catching and fielding can create momentum and save a team the 5, 10 runs that win the game. Nepal were uncharacteristically poor in the field against Italy and West Indies, often fumbling and leaking boundaries. Airee didn’t get any of his usual run-outs either. Nepal lost cheap wickets through run-outs and stumpings. All these unforced errors right through the match add up on the scoreboard.  <figure><img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20260218010220_1630c283f277631dfbddd3d7f29b930b124bde97c8f6a411cc2e1d089e452f45.jpg" data-media-id="editor_4" data-image-id="20260218010220_1630c283f277631dfbddd3d7f29b930b124bde97c8f6a411cc2e1d089e452f45" data-rendition-name="original" width="1366" height="2048" loading="lazy" alt="T20 World Cup Nepal"></figure>  SKILL SET Mentality is important but sport performance ultimately comes down to skill. There looked to be a large gap, and perhaps one of the reasons is because the Nepal team is so full of all-rounders. Airee’s two-way performance is undeniable, but Bhurtel, Paudel and Karan KC do plenty of both too and they do not do it super well very often. If the team wants to get consistent, it must have consistent performers with the bat and ball. That calls for some of these players to focus completely on one skill over the other. You do not see openers bowling so much in the top teams as Bhurtel does. The main reason for this skill gap, and one of the hardest parts about being an associate nation, is how little cricket the members of the team play compared to the test nations. Said Stuart Law: “The longer format is where you learn how to play the game. The shorter formats are where you have your fun. We need some sort of multi-day games.”  <figure><img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20260218010220_652ef3ba6fceab394a94c18cabd322dca8ba4a1266557660064339de9169c91d.jpg" data-media-id="editor_5" data-image-id="20260218010220_652ef3ba6fceab394a94c18cabd322dca8ba4a1266557660064339de9169c91d" data-rendition-name="original" width="2048" height="1366" loading="lazy" alt="T20 World Cup Nepal"></figure>  The contrast in experience showed during the Italy game. Most of the members of the Italy team were well into their thirties, had played a high volume of domestic cricket and were more self-assured. So, while the young Nepali team were more athletic, they seemed to lack the skill and experience to know what to do when things were going wrong. The Italians seemed to go about their game with a lot more self assurance. In the long run, this means setting up grassroot structures, getting kids into formal training when young, and setting up a longer format domestic league. In the short term, CAAN could organise frequent series with other associate nations, and individual athletes could go play long form club cricket abroad. Surely some team in the world has to have a spot for a player like Airee, for example. It has been Airee’s tournament. Scores of 44 v England, 58 v West Indies, and now a match-winning 50 against Scotland that gives the travelling Nepali support something to cheer for. The tournament could have been a lot more, but it is wholesome to end on a win.

Nepal goes in and out of T20

The recent Nepali Times Substack post titled ‘Unresident Nepalis’ made me realise I also belong to the category of Nepalis who are technically Non-resident Nepali (NRN), but want to ‘permanently reside inside Nepal’.&nbsp;
Although this was meant as a joke, it is ironic that many of those who go abroad long to come back home, and those who have not emigrated cannot think of a good enough reason to stay back in Nepal.&nbsp;
As soon as the NRN Citizenship was officially introduced in late 2023, I had tried to apply for one but was shut down before even submitting my documents as the district administration office firmly told my then lawyer that I needed to prove “तिन पुस्ता” proof of three generations of Nepalis from my father’s side.&nbsp;
My late father was from Japan and relinquished his citizenship to become a Naturalised Nepali citizen in 2006. Three years ago, I dismissed the rejection with the thought that I will try again later when government officials would gain more experience with such applications.&nbsp;
Now, with an ailing mother and an energetic toddler, I felt the need to act soon and reached out to a law firm that specialises in NRN citizenship applications. To my surprise, they were positive after reviewing my documents, although they did warn me that we may need to overcome some obstacles.&nbsp;
In 2023, I had applied in the district office where my father had received his naturalised citizenship, but now the suggestion was to try from the district where my mother had received her Nepali ancestral origin “बंसागज” citizenship.&nbsp;
The lawyers pointed to the NRN citizenship mandate which clearly states that it can be acquired via a Nepali origin father, mother, grandfather or grandmother. The firm helped arrange the necessary documents required and the first step was to get a “सिफारिस” &nbsp;recommendation letter from my mother’s ward office.&nbsp;
This was the first hurdle as the ward office was unsure if they could issue such a letter, so they checked in with their head office, and luckily we received the go ahead. After persistent follow up from the law associates, they were able to provide us with a recommendation letter and we filled out the application forms.&nbsp;
The law firm wisely suggested that I take the paperwork myself to my mother’s district office while they stayed in the background in case I needed help explaining my situation.&nbsp;
With a big smile and cheerful tone, I dutifully followed the process and to my surprise, I found most of the officials ready to help without creating unnecessary hurdles. The application has to be signed off by the Chief District Officer (CDO) or Assistant CDO and just when I thought wow, I am going to breeze through this, one officer noticed that my father’s naturalised citizenship was from a different district and told me that I should apply for my NRN from there.&nbsp;
I explained that my father has already passed away and as he was not originally a Nepali, therefore it is not possible for me to get my NRN from his documents, as the requirement is ancestral “बंसागज” citizenship. The officer then went to check with their seniors and later told me that I would need police verification as an extra precaution.&nbsp;
Off I went to the police headquarters where they issued a sealed letter to be given to the police station that was in the same vicinity as my mother’s ward office. At the station I was told to get four people who are not my relatives to testify our documents are true.&nbsp;
This process happened to be more stressful than dealing with the government offices. At first, it turned out that most of my mother’s old neighbours had already passed away or had citizenship papers from another area. Others confirmed their availability, but later had conflicting schedules. Luckily, one very helpful old neighbour was able to arrange for enough people to verify the documents.&nbsp;
Encouraged that the end of the tunnel was in sight, I went back to the district office with all the requested documents, and after some initial pushback, I was finally referred to meet the official who signs off the documents before it goes to the CDO.&nbsp;
As luck would have it, the officials were in a meeting that lasted more than two hours, and I had to give my mother her insulin shot and noodles from the cafeteria in the waiting area.&nbsp;
When we were finally able to meet the officer, he didn’t even look at my papers properly and started questioning my lawyers whether they had even read the law, how could I apply for Nepali citizenship when I already had a Japanese passport, etc. He somehow assumed that I was looking to get a normal Nepali citizenship from my mother’s side, and we informed him that I was only looking to get an NRN citizenship, after which his tone became more apologetic and said that he would need to look into the law more closely.&nbsp;
It had already been three full days of working through each step of the process, and I had no problem waiting another day for the conclusion.&nbsp;
Perhaps because this NRN citizenship is a fairly new law and perhaps a lot of NRNs apply from the Nepal’s embassies in their country of domicile, throughout my experience, officials kept on telling me that a case such as mine has not been processed before.&nbsp;
My case being that I have never had a Nepali citizenship, my father having a naturalised Nepali citizenship and my mother being the only 100% Nepali in the family. I kept on saying that just because it has never been done before does not mean that it cannot be done, and sure enough, the next day the officer signed off on my documents, even kindly saying that they should have highly respected my application upon learning about my late father and his contributions to Nepal.&nbsp;
Although the intricacies of the NRN citizenship law have not been fully hacked out such as the transfer of land ownership, it is definitely a positive step in securing the rights and aspirations of fellow NRNs as many would agree that no matter where we go, “यो मन त मेरो नेपाली हो!”&nbsp;
Sonia Miyahara, Managing Director of Hotel Everest View, Trans Himalayan Tours &amp; Trekking Pvt Ltd &amp; Himalaya Kanko Kaihatsu Co. Ltd.

How I got my NRN Citizenship in Nepal

After his critically acclaimed 2023 book of essays सुन्यताको मुल्य on the state of women and children in the <a href="https://nepalitimes.com/banner/the-karnali">Karnali</a>, paediatrician and writer Nawaraj KC has come out with a next one, Swasparsh. The new book is almost a sequel to the first one, with real-life stories drawn from his medical practice and social engagement. Both are powerful accounts of suffering, resilience, and the search for human dignity in Nepal’s most remote and underserved districts. The book opens with deeply disturbing yet real incidents of the suicide of a Grade 2 student. A &nbsp;frantic mother rushes in with a son who had already written a suicide note but was saved at the last moment. There is a desperate call from a young woman threatening to jump into the Karnali River.&nbsp; We meet children carrying immense trauma: a toddler who refuses to eat after losing her mother, and another child who stops speaking after experiencing sexual abuse within the family. The emotional climax comes when KC himself falls into depression after being violently attacked by a drug addict patient, leaving him with a serious head injury.&nbsp; But this is not a book of only sad stories of deprivation and poverty. It is how people who find themselves in the worst circumstances struggle to overcome what life has thrown their way, and triumph in the end. By just surviving against all odds, people emerge stronger, often with a renewed commitment to helping others. As a paediatrician working out of his native Surkhet in Karnali Province, KC's work brings him face-to-face with the human side of what a centralised government’s neglect and apathy can do to communities in <a href="https://nepalitimes.com/banner/no-dasain-in-kalikot">Nepal’s most far-flung region</a>. KC shows empathy not just to human beings in trouble, but also animals and underlines the importance of coexisting with the natural world. By helping others individuals ultimately help themselves. Although a paediatrician by profession, KC demonstrates a deep understanding of structural oppression, gender discrimination, caste hierarchy, class inequality, and regional marginalisation within the Nepali state.&nbsp; He also captures moments of tenderness, such as young couples supporting one another through hardship. How poverty can drive families to take heartbreaking decisions — like a patient forced to discontinue life-saving medicine in order to qualify for disability allowances needed to repay debt.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20260217030252_ffd67815063cffe51a0310f10405a554f6094ba05564993f34086fe4b31543f6.jpg" data-media-id="editor_2" data-image-id="20260217030252_ffd67815063cffe51a0310f10405a554f6094ba05564993f34086fe4b31543f6" data-rendition-name="original" width="1646" height="2048" loading="lazy" alt="Swasparsha"> </figure>  A former teacher is forced to beg despite receiving treatment, exposing the failure of conventional development models that ignore sustainable livelihoods.&nbsp; Then there are inspirational stories like the one of Mandire, who ran away at age 12 to work as a labourer in India, suffered severe burns while unloading coal, and lost a hand. Despite this, his infectious smile and fortitude transformed him into a local symbol of hope both in India and Nepal.&nbsp; Even in old age, he is always smiling and helping others less fortunate.&nbsp; Through Mandire’s story, KC explores the science of the healing power of a smile, the positive psychology of a ‘mental gymnasium’ in which optimism is cultivated through conscious practice.&nbsp; For example, a young girl from the historically marginalised Badi community which faces deep social exclusion refuses to accept her circumstances, and grows into an advocate for other disadvantaged children. A devoted foster mother dedicates her life to raising orphans, empowering them despite her own hardships. One of the book’s strengths lies in its accessibility. In Nepali language, KC blends science, philosophy, and lived experience into everyday language that resonates with villagers and ordinary readers. He comes across not only as a doctor and healer, but also as a teacher, nature lover, and social activist. He tries to introduce greenery to a remote school, and how this transformed children’s learning experience. He reflects that his patients are his greatest teachers helping to expand knowledge beyond medicine and technology into the realms of humanity and ethics. I read Swasparsh after witnessing the recent GenZ movement. The book’s recurring calls to youth, appearing at the end of several chapters, has special relevance today. KC reminds young readers that hardship is part of everyday life, but within struggle lies the potential for healing and growth.&nbsp; He encourages self-reflection, self-healing, and cultivating a positive mindset. Above all, he asserts that humanity’s greatest gift is its own human capacity henceforth solutions to all problems lie within oneselves rather than outside forces. The GenZ movement represents an urban youth revolt against traditional political parties and state institutions that have failed to deliver opportunities and accountability. Rising unemployment, widespread corruption, and frustration with stagnant governance have fuelled demands for new political alternatives.&nbsp; With the 5 March election less than three weeks away, many young people hope that new forces will be capable of bringing systemic change. Yet whether these forces can truly meet their aspirations remains uncertain. Established political actors are reluctant to relinquish power, while emerging groups often lack organisational depth and historical experience. In many ways, these new political actors resemble the people of Karnali: resource-poor, And in the periphery of power, yet rich in commitment and determination. Drawing from Buddhist teachings that recognise suffering, understanding its causes, and seeking pathways to overcome it, KC indirectly inspires today’s youth. Every problem contains the seeds of its own solution, provided we learn to know ourselves, care for ourselves, and care for others. Ultimately, the title Swasparsh means self-healing, self-reflection, and self-confidence. At a time of political uncertainty and generational change, this book speaks directly to Nepal’s younger and the emerging alternative forces — reminding them that transformation begins from within.&nbsp;  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/2026021704020_1d2a855730bc14acbea596cce7b3a00b20f85c79c3a7d8ca46274a15eb642f59.jpg" data-media-id="editor_3" data-image-id="2026021704020_1d2a855730bc14acbea596cce7b3a00b20f85c79c3a7d8ca46274a15eb642f59" data-rendition-name="original" width="1136" height="702" loading="lazy" alt="Swasparsha"> </figure>  Hisila Yami served as CA member, Minister of Physical Planning &amp; Works, Minister of Tourism &amp; Minister of Land Reform. At present, she is a member of Central Political Council in Pragatishil Loktantrik Party and is a lecturer in IOE Pulchok.

Essays on self-realisation and self-healing

Besides being an election year in Nepal, 2026 is also the year of anniversaries. It is exactly 30 years since the Maoists launched their armed struggle on <a href="https://nepalitimes.com/editorial/13-february">13 February 1996</a>, and it was on 27 April 2006 that the ceasefire came into effect after a month of massive pro-democracy protests.
Alas, <a href="https://nepalitimes.com/editorial/not-ever-again">three decades on</a>, the decade-long conflict that claimed 17,000 lives has been <a href="https://nepalitimes.com/banner/ghosts-of-war">air brushed from our history</a>. For the survivors, and the families of those disappeared and killed, memories of loss and suffering are fading. The party that fought the war in Mao’s name has dropped it.
It is important on this day to remember not to forget that <a href="https://archive.nepalitimes.com/news.php?id=3203">violent decade</a> -- so that it does not happen again, and so the youth movement that has led to this election will also not be in vain.
The 8 September 2025 rally, <a href="https://nepalitimes.com/news/nepal-s-8-september-massacre">the massacre that followed</a>, and the nationwide mayhem and carnage the next day were largely a result of public anger boiling over. Nepalis had been let down repeatedly by rulers promising revolution in the name of the ‘people’: from the 1990 People’s Movement I, to the Maoist ‘People’s War’, and the 2006 People’s Movement II.
There are some positive residual effects of the insurgency. One-third of the Maoist militia was <a href="https://archive.nepalitimes.com/article/nation/Nation-sibling-war-juna-rai,731">composed of women</a>, this empowered not just the female guerrillas themselves, but indirectly made a whole generation of young women aware of their rights.&nbsp;
The peace process itself resulted in the Maoists entering the democratic mainstream, and the induction of many of the guerrillas into the national army – a rare occurrence after a conflict.
The ceasefire was followed by an interim government, and the first elected <a href="https://nepalitimes.com/editorial/the-letter-and-spirit">Constituent Assembly</a> abolished the monarchy in 2008. Deadlock over the model of federalism meant a second election had to be held in 2013, and the new Constitution <a href="https://archive.nepalitimes.com/regular-columns/by-the-way/new-constitution-should-adopt-inclusive-democracy-with-federalism-republicanism-secularism,538">finally promulgated in 2015</a>.&nbsp;
That statute was supposed to devolve political decision-making away from Kathmandu to autonomous provinces, improve inclusive representation of women and hitherto excluded castes and ethnicities at all three levels of government, ensure accountability and good governance to generate jobs and lift living standards.
There were seven governments in ten years after 2015, and tottering coalitions one after another failed to fulfil any of those provisions in the Constitution. There were subliminal gains in representation of women thanks to affirmative action, but as this election shows, women candidates are still used as proxies by patriarchal parties.&nbsp;
Since the two warring sides of the Maoist war both became the state, sharing power in dozens of coalition cabinets since 2006, they colluded to bury the <a href="https://nepalitimes.com/news/nepal-s-unpunished-war-crimes">transitional justice process</a>.
The former supreme commander of the Maoists Pushpa Kamal Dahal (Prachanda) has become prime minister three times in the last 20 years. He is contesting this election from Rukum East, where he marked the 30th anniversary of the start of armed struggle on Friday.
The word ‘Maoist’ has been erased from the Nepali Communist Party which Dahal formed with more than a dozen other smaller leftist outfits. His main rival, Janardan Sharma, quit the Maoists and is standing for elections in Rukum West.
Both former comrades are competing for the hearts and minds of people of this former base area from where the Maoists went on warpath on 13 February 1996 by attacking a police station in Athbiskot, and simultaneously on targets in <a href="https://archive.nepalitimes.com/news.php?id=7812">Holeri of Rolpa</a>, Sindhuli and Gorkha.
The former ideologue of the Maoist party, <a href="https://archive.nepalitimes.com/article/editorial/20-years-wasted-in-war,2850">Baburam Bhattarai</a>, was the architect of the revolution while Dahal was the <a href="https://archive.nepalitimes.com/news.php?id=6369#.Y-XIii8w1KM">executor</a>. Bhattarai submitted a list of 40 demands to the <a href="https://nepalitimes.com/editorial/deubas-denouement">Sher Bahadur Deuba</a> (during his first tenure as prime minister in 1995) but did not wait for a reply before launching the armed struggle.
The Maoists felt that the constitutional monarchy after 1990 was too feudal, and a patronage-driven parliamentary system too slow to bring about change. Besides, the democratic parties were accused of using state security to prevent Maoist candidates from winning elections.
The Maoists followed Mao’s Red Book to the letter, attacking police stations, looting weapons and targeting local elected governments, eliminating ‘class enemies' with summary executions.&nbsp;
They destroyed telecommunication towers, highways, bridges and airfields in remote areas. Threats forced health posts, schools, post offices to be withdrawn from areas where people needed them the most. The country’s development was pushed back decades.
Nepal in the early 1990s was ripe for revolution. There was inequality, social injustice, exclusion, and the political parties in Kathmandu were too busy squabbling to do their job. The Maoists wanted an end to the monarchy, but in 2001 the monarchy imploded with the royal massacre.
ABSOLUTE POWER
King Gyanendra succeeded his <a href="https://archive.nepalitimes.com/news.php?id=8338">murdered brother</a> to the throne, and took the country back to absolute rule with a military-backed coup in 2005. Within a year, street protests forced him to step aside. And by 2008, it was too late to save the monarchy.
We can look back as far as we want to the roots of the Maoist conflict. It can be blamed on elected leaders post-1990 who abandoned the people once in power, the 30 years of partyless Panchayat system that stifled dissent and let social pressures build up, or even 100 years of Rana rule.&nbsp;
It was the prolonged indifference on the part of successive rulers in Kathmandu that fed public discontent. These accumulated grievances were also the reason for the <a href="https://nepalitimes.com/news/nepal-s-gen-z-protest-turns-deadly">September 2025 events</a>.&nbsp;
During China’s Cultural Revolution, Mao Zedong said: ‘The old has to be uprooted to be replaced with the new’, and that could almost be the anthem of the GenZ movement and this election.
The objective conditions that drove the Maoist insurgency 30 years ago are still evident today. And much will depend on the government(s) that will be formed after March.&nbsp;

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