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 greening of the Khumbu

Climber, expedition leader and later a supplier of bottled oxygen to Himalayan mountaineers, Henry Barclay Todd died on 3 November 2025 in his favourite place on earth, Kathmandu.&nbsp;
Todd was larger than life, a metaphor often used, yet it could not be more fitting. Standing nearly 2m tall, and possessing an unshakeable will, he lived life on a grand scale, both in body and spirit.&nbsp;
Todd was a pillar in the Himalayan climbing community, supporting many mountaineers across Nepal and Pakistan, making it possible for them to fulfil the dream of standing on the world’s highest peaks. He believed deeply in the strength, skill, and potential of the Sherpa people, and offered them opportunities that might otherwise have remained out of reach.&nbsp;
“Thank you, Henry. Your trust changed my life. Rest in peace, my leader, my teacher, my friend,” said Dorjee Gyelzen Sherpa in his tribute.
Born in 1945 to Royal Air Force officer Henry Todd and May Todd of the Women’s Royal Air Force, Henry spent his early years in Singapore. He led a lively childhood with his two brothers, far removed from the mountains that would later define his path.&nbsp;
A gifted swimmer like his father, Henry never pursued the sport professionally. Instead, after returning to Dundee as a teenager and attending seven different schools, he set off for London, where he began working for an insurance company before finding his true calling in adventure.
Henry Todd first came to Nepal in the mid-1980s and made his first attempt on Ama Dablam in 1987, an expedition that marked the beginning of an extraordinary and colourful climbing career. <a href="https://www.himalayandatabase.com/" target="_blank">The Himalayan Database</a> lists 61 expeditions that he led in Nepal alone — there were more in the Karakoram, Argentina and the Alps.&nbsp;
But Todd would joyfully say that a few hard Scottish ascents held a more personal meaning to him than even the greatest Himalayan summits.
Over the decades, he crossed paths with many legendary climbers like Anatoli Boukreev, Jerzy Kukuczka, Doug Scott and Chris Bonington as well as celebrities including members of Pink Floyd and Nobel Prize laureates whom he befriended.&nbsp;
He had a gift to never name-drop, but would simply mention that he had had lunch with Minnie Driver (niece of his long-time friend Andra) or that he had bought his first car from Donald Sutherland. For Todd, these were not bragging rights, they were simply part of the colourful tapestry of his life.
Todd’s life was filled with extraordinary experiences from surviving plane crashes, avalanches and earthquakes to quietly solving countless problems, which was one of his favourite past-times. His hands, famously large and steady, were always ready to help whether in the chaos of the mountains or the calm of a base camp.&nbsp;
With his sharp sense of humour and the beloved exclamation “Whoopie!”,he could bring lightness even to the toughest moments. He never tired of taking on challenges or helping when someone was in need, and he enriched so many people’s lives with his endless stories.
His legacy is immense. He helped build the human backbone of Himalayan climbing, enabling generations of climbers to test themselves in the world’s highest places. With his passing, an era of bold, spirited Himalayan guiding has come to a close.
Todd survived by a loving family, many close friends and a global community of climbers and Sherpas who will never forget him and his endless tales.&nbsp;
His family said in a statement: ‘Henry’s strength, warmth and unyielding belief in others will live on far above the clouds. He was indestructible in our eyes and in our hearts, he always will be.’
There will be a memorial service at Pashupati Temple in Kathmandu on 8 November 2025 around lunchtime.

Henry Barclay Todd, 80

The autumn mountaineering season is not over yet, and already there have been 12 fatalities on Himalayan peaks in Nepal.
Of the 1,450 climbing permits issued, 436 were for Mt Ama Dablam (6,812m), 374 for Mt Manaslu (8,163m) and 186 for Himlung Himal (7,126m). There were deaths on all three mountains.
The death of two French climbers on Ama Dablam happened before unseasonal blizzards hit the mountains. But Cyclone Montha from the Bay of Bengal brought on high winds and up to 1m of snow in the peak trekking and mountaineering season.
This increased avalanche conditions, and made helicopter evacuation of stranded and injured climbers difficult. Lower down the mountains, more than 1,000 trekkers from Nepal and around the world were stuck in the Annapurnas, Manaslu circuit and the Khumbu.
However, there have also been allegations that it was not just the weather that delayed rescues. Multiple levels of bureaucracy and the need for flight permits to restricted areas like Manang and Manaslu critically delayed evacuation flights.
Italian climbers Farronato Stefano and Caputo Alessandro were found dead in their tent at Panbari Himal Camp I (6,887m) in the Manaslu area. They had been trapped by heavy snowfall since 28 October, and their bodies were found on 4 November by a team from the expedition organisers, Sherpa Alpine Trekking Service. The team was made up of high level mountain guides and expedition leader Valter Perlino.
The team had been climbing to Camp 3 but decided to descend to base camp because of thrombosis in Perlino’s left foot. The two climbers who would eventually get trapped decided to break at Camp I, a decision that would prove fatal after the projected six-day snowfall arrived two days early.
“They were sleeping in a tent and were buried under 2.5 metres of compacted snow. It happened during the night between Thursday and Friday. While they were sleeping, absurd,” said Perlino.
A deadly incident took place the morning of 3 November, when five foreigners and two Nepalis died in an avalanche on Yalung Ri at 5,630m in the Rolwaling. They were part of a larger group of 15 that were acclimatising for an attempt on the nearby Dolma Khang (6,332m).
Local authorities in Gauri Shankar Conservation Area say calls were immediately made to helicopter companies as well as various ministries in Kathmandu that have to issue permits to fly to the region bordering China.
But the permits for rescue flights to Rolwaling Valley were delayed by eight hours. Rescue flights in these areas require permission from the Ministry of Tourism, the Ministry of Defence, the Home Ministry, and the Civil Aviation Authority of Nepal (CAAN).
Experts say this should be exempted in times of emergency when time is of the essence. CAAN spokesperson Pratap Babu Tiwari claimed to not know of the avalanche on Yalung Ri and deflected questions to the permission department.&nbsp;
There was a similar tragedy on Himlung Himal in Manang as well. Australian Chin-Tark Chan, 49, was climbing with 8K Expeditions and fell ill on 27 October at about 6,800m, developing snow blindness and loss of mobility. The guides immediately called the US insurance company Global Rescue for authorisation of a longline rescue.
Global Rescue refused, saying a rescue at that height would violate Nepal’s aviation rules and put the pilot at unacceptable risk. They asked the guides to transport Chan to Camp 3 at 6,400m to a permitted altitude. Seeing it was a life-or-death situation for its client, 8K called in an aerial rescue anyway, but the helicopter could not land due to bad weather. Chan died slightly below Camp 3 on 29 October.
Global Rescue said in a statement that it was ready to send in a helicopter after Chan had been transported to Camp 3, but several hours were lost for that attempt, and the weather did not get better in the next few days.
To underscore just how dangerous helicopter rescues in the Himalaya can be in bad weather, a chopper from Altitude Air skidded off the helipad at Lobuche below Mt Everest while trying to rescue trekkers in whiteout conditions.&nbsp;
CAAN announced a ban on flights during blizzards or dense fog. While rescue missions are often heroic and courageous, they should not be foolhardy if conditions are unsafe and the risk to pilots and rescuers too high. This autumn was a lesson for future expeditions and for the Nepal government.&nbsp;
The Italian duo on Panbari were caught out by snow that arrived two days ahead of schedule, but the group on Yalung Ri should have postponed their ascent after multiple warnings from the Department of Hydrology and Meteorology to avoid high altitudes.

Deadly autumn in Himalayan climbing

Traditional donors have sharply scaled back their aid commitments to developing countries over the past year. Some, like the United States, have virtually eliminated their aid programs. According to the Organisation for Economic Co-operation and Development (OECD), official development assistance (ODA) from member countries <a href="https://www.oecd.org/en/about/news/press-releases/2025/04/official-development-assistance-2024-figures.html" target="_blank">declined by 7.1%</a> in 2024, its first annual drop in six years. This trend was not limited to a few major donors. Of the 33 members of the OECD’s Development Assistance Committee (DAC), 22 slashed their aid budgets, and only four countries met the United Nations’ target of allocating 0.7% of gross national income to ODA. The outlook for the coming year offers little hope for improvement, as major DAC donors have announced additional cuts. Most notably, US President Donald Trump’s administration has suspended most foreign aid and dismantled the Agency for International Development (USAID), which dispersed most US government aid dollars. Meanwhile, the United Kingdom plans to <a href="https://www.bbc.com/news/articles/clyrkkv4gd7o" target="_blank">reduce aid spending</a> from 0.5% of GNI to 0.3% by 2027. Similar retrenchment across Europe and North America is reshaping international assistance, disrupting humanitarian and climate-related programs, and creating financing gaps in critical sectors such as health, education, and clean energy. In our 2017 book <a href="https://www.cambridge.org/core/books/going-beyond-aid/B48F59C6D8D2790D403A1A0C44B37612" target="_blank">Going Beyond Aid</a>, we urged developing-country governments to reduce their dependence on foreign aid, not only because it was becoming an unreliable source of funding, but also because other, better ways of financing development were becoming more available. That message is more urgent than ever. As reliance on aid becomes untenable, the international community must mobilise a broader array of financing sources to advance green and sustainable growth. This includes national development banks, industrial investment funds, sovereign wealth funds, and institutional investment in public markets, as well as innovative mechanisms such as debt swaps and public-private partnerships (PPPs). These tools can unlock domestic resources, attract long-term investors, and create synergies between public goals and private capital. Equity investment offers a promising avenue for engaging non-traditional development partners while reducing developing countries’ dependence on debt. Government investment funds, public and private financial institutions, and other private actors can participate by taking equity stakes in public enterprises, financing infrastructure projects, or joining PPPs. Such participation not only alleviates debt burdens but also improves the performance and management of public assets. As government-funded, mission-driven institutions, public development banks (PDBs) have the potential to provide patient capital for green and sustainable investment in emerging and developing economies (EMDEs). Building on the <a href="http://www.dfidatabase.pku.edu.cn/index.htm" target="_blank">pioneering database</a> of public development and financial institutions created by the Institute of New Structural Economics at Peking University, future research can identify effective ways to harness these institutions to fuel low-carbon growth. Responding to growing demand from the economies of the Global South, development partners have increasingly adopted an “entire value chain” approach to the green transition in recent years. This strategy facilitates transfers of low-carbon technologies, diffusion of digital innovations (including trade in services), and industrial modernisation, enabling countries included in China’s Belt and Road Initiative (BRI) to accelerate their shift toward sustainable development. Empirical research supports this approach. An analysis covering 139 countries <a href="https://ember-energy.org/latest-insights/the-first-evidence-of-a-take-off-in-solar-in-africa/" target="_blank">finds</a> that, following policy directives to incorporate green and low-carbon principles into the BRI, carbon intensity (CO₂ emissions per unit of GDP) among participating countries declined significantly between 2013 and 2022. These findings are consistent with another <a href="https://ember-energy.org/latest-insights/the-first-evidence-of-a-take-off-in-solar-in-africa/" target="_blank">recent study</a> showing how China’s solar-energy expansion has helped transform Africa’s power sector. Investment in infrastructure and industrial development can also generate positive spillover effects. Evidence from Sub-Saharan Africa <a href="https://onlinelibrary.wiley.com/doi/full/10.1111/jors.70023" target="_blank">shows</a> that the presence of at least one Chinese-financed infrastructure project in a second-order administrative region (comparable to a municipality) is associated with a 5% increase in nighttime luminosity – a widely used proxy for economic activity. Neighbouring regions experienced a 10-15% rise in luminosity, indicating that the benefits of such projects extend well beyond the immediate investment site.  <figure><img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20251104131124_1a11d248a89b0785bc7d7f1d9f721e7e7a2563cbd579c3c672a0900220c19171.jpg" data-media-id="editor_7" data-image-id="20251104131124_1a11d248a89b0785bc7d7f1d9f721e7e7a2563cbd579c3c672a0900220c19171" data-rendition-name="original" width="720" height="405" loading="lazy" alt="development aid and China"></figure>  These outcomes underscore the critical role of infrastructure investment, particularly in energy and transportation projects. By improving electricity access, affordability, and connectivity, they reduce energy poverty, bolster public services, and stimulate economic activity in underserved areas. To meet the evolving challenges of development finance, both traditional and non-traditional donors and creditors should move beyond aid and adopt multidimensional strategies that combine trade, investment, infrastructure, green technology, and digital connectivity, including fintech solutions, to support EMDEs. Importantly, such collaborations should be viewed as a mutual learning process in which partners assume complementary roles and shared responsibilities. To be sure, there have been missteps along the way. China’s financing of coal-fired power plants before 2021, for example, had slowed reduction in CO₂ emissions. But these outcomes, once recognised as policy errors, can help strengthen accountability and foster self-correcting mechanisms within the international development ecosystem. Through ongoing learning and adaptation, global partners can build a more resilient, inclusive, and sustainable framework for development finance. © <a href="https://www.project-syndicate.org/">Project Syndicate</a> Justin Yifu Lin, a former World Bank chief economist and Senior VP, is the honorary dean of the National School of Development and director of the Institute of New Structural Economics at Peking University. Yan Wang is Senior Academic Researcher at Boston University’s Global Development Policy Center.

Development finance must shift away from aid

This is the 73rd episode of Diaspora Diaries, a Nepali Times series in collaboration with Migration Lab providing a platform to share experiences of living, working and studying abroad. I don’t remember playing with dolls as a little girl. There is not much to remember from my childhood.&nbsp; My responsibilities began at a very young age, as I had two younger brothers to take care of. I was born in Sarlahi, but we moved around quite a bit as my father was in the government and got transferred frequently.&nbsp; From Rasuwa to Dang, from Nepalgunj to Kathmandu. I struggled to adjust in Kathmandu because I joined Grade 9 in the middle of the term. The education was different and fellow students also did not support me initially. But over time, I adjusted and made friends. I did not dream of becoming a nurse. It was by accident. I wanted to pursue medicine, but failed the entrance exam by a few marks. I did not want to lose a year, so decided to take up microbiology instead.&nbsp; I got married after my undergraduate, and my husband encouraged me to take up something more technical like nursing or engineering instead of Masters in Microbiology. As my quantitative background was weak, I chose nursing. I felt like I was born to be a nurse. Juggling my married life and studies was difficult. My teachers would often ask me why I am falling behind. It was not easy, but I managed and took up a full-time job as a nurse. There are challenges being a nurse in Nepal. You are overworked, underpaid, there is lack of appreciation. Superiors can be overbearing. These problems persist. But the bright spot is that you get to serve fellow Nepalis, and be close to your family.&nbsp; Just like I had no intention initially of becoming a nurse, I had no intention of migrating overseas. But life had different plans for me. After my baby boy was born, I noticed that something was off. Even at nine months he had not started crawling or sitting. As a nurse I knew something was wrong, and I took him for check-ups. He tested negative for down syndrome, but he had a heart defect.&nbsp; The cardiologist recommended that I take him to India where he was diagnosed with Williams Syndrome, a rare genetic condition that affects 1 in 10,000 people. It delayed his development. I looked for therapy. It was either not effective, or too expensive. Some schools also refused to admit him, and it drove me to tears.&nbsp; My family members overseas in the UK, US told me to emigrate as there were better facilities for differently abled children. So I decided to apply to the UK. Luckily just then there were calls for candidates under the Nepal-UK government-to-government pilot scheme for 100 nurses. Only 40 met the criteria, and I was one of them.&nbsp; I still remember the day I received the news on the day of my puja. There were people around me, and they told me that it was the result of my fasting and devotion on that auspicious day. Perhaps it was. Life was taking a new turn, and I was happy. I made it to the UK in February 2024 without paying a single paisa to any broker. The G2G scheme was unique as we were treated with dignity and valued for our skills: they covered costs for the ticket and visa, reimbursed us for exams we had taken and costs involved in the preparation and testing of the Objective Structured Clinical Examination were also covered.&nbsp;  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20251106071148_dc5a0d0ea3024b34a4f2735754f8eb67a650bc7f61b98c75d589676c65b02a0c.jpg" data-media-id="editor_0" data-image-id="20251106071148_dc5a0d0ea3024b34a4f2735754f8eb67a650bc7f61b98c75d589676c65b02a0c" data-rendition-name="original" width="1200" height="1600" loading="lazy" alt="Nurses NT"> </figure>  It was of course difficult to leave my son behind. But I was doing it for his future. I had the option of taking him from the start, but it was a new place and I wanted to be well-settled and knowledgeable about the options available for him before bringing him along. As I packed, he would ask me to take him with me in my suitcase. It did not seem like he was affected by my departure, and it was only later that his teachers said that he would express his feelings more openly at school. He just did not know how to tell me he missed me, and he would tell teachers he was worried I had forgotten him if we did not speak for a day.&nbsp; He missed me, and that realisation made me emotional. But I had to carry on. Life in the UK was difficult in the beginning. Even so, I wanted to prove to myself that I could do it. Fortunately I had cooperative staff who patiently answered my questions. I think I would have been irritated if I were in their place. But they did not seem to mind, and their support and guidance made it easy for me to adjust to the new work environment. APPRECIATION I still struggle to understand the accent of my English patients, and have ask the matron for help. They compliment me on my English, but I can speak better than I understand. The good thing about working in the UK is that you are appreciated for your work, which can be motivating. Sometimes, after a long day’s work you get a message from your supervisor acknowledging your work with a thank you. That’s enough to erase your tiredness.&nbsp; So far I have received 32 WOW nominations which are acknowledgements from patients for a job well done. It can be motivating, especially in the beginning. The main difference between the Alpana who first left Kathmandu for the UK and the Alpana now is that I am a much more confident person. What makes a good nurse? Skills, knowledge and qualifications are of course a given. But mostly, you need humanity. A smiling face. The way you communicate. Your empathy. These attributes can already solve many problems that patients are facing. This is my second time back home in the last 20 months. And this time, I have arranged for my son’s visa. I will go back after Tihar with my son and husband.&nbsp; I am happy, but also a little nervous about what awaits us. What kind of school will I put him in? Will it really be different from schools here? Will his needs be addressed? Will it be like here, or will he be able to adjust?&nbsp; But I am determined to make it work. Success for me would be if he adjusted well and there is a change in his condition. He still cannot recognise alphabets and read words like kids in his age group. Hopefully he will get learning support in the UK. He also has a knack for music, and this is common among individuals with Williams Syndrome. His ears perk up when he hears music, and he takes part in musical events at school. He still does not recognise letters &nbsp;but he uses voice commands to search for guitar videos on YouTube. I will enrol him in music classes, and help him develop this gift. For now, I worry how he will behave on his long flight. He has a short attention span and gets restless. He is also very social and will want to speak with everyone around him, and might irritate fellow passengers.&nbsp; I have already started trying to make him understand that he will need to behave on the flight. He nods in agreement. Let’s see how it goes. &nbsp;

glacier-melt

Meltpools in the Himalaya

The greening of the Khumbu

Henry Barclay Todd, 80

Deadly autumn in Himalayan climbing

Development finance must shift away from aid

“I felt like I was born to be a nurse”