Thursday, August 14, 2025

Surging Himalayan rivers bring benefits and risks to local communities



Melting glaciers are raising river levels and impacting hydropower



American Geophysical Union

Flow changes in rivers of High Mountain Asia 

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The average percentage change in river discharge, or river flow, per year, is increasing over much of High Mountain Asia. Red and orange represent decreases in river discharge and blue represents increases in this map of the Himalayas, Karakoram, Pamir and Tian Shan. The inset maps depict the detailed measurements of the new study, down to 5-mile segments.

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Credit: Flores et al, AGU Advances https://doi.org/10.1029/2024AV001586





WASHINGTON — Rapidly melting glaciers are surging water volume in at least 10% of rivers in High Mountain Asia, including large rivers like Yangtze, Amu Darya and Syr Darya, according to a comprehensive new study of the region. In parts of upstream rivers, water flow nearly doubled over the course of a decade. Communities that depend on the rivers for power could benefit from the increase in river power, but additional sediment carried in the water may clog infrastructure. The increase is currently found specifically in upstream parts of the rivers, but downstream communities could face the same outcome as glaciers continue to melt.

Encompassing the Himalayas and the Hindu Kush and powerful rivers like the Yangtze, Yellow and Indus, High Mountain Asia is a complex geographic region that supplies water to around two billion people. The rivers are primarily fed by glaciers, snow and rainwater, but the river systems are changing as a result of climate change impacting temperature, monsoon season and droughts. Previous research has projected the glaciers in High Mountain Asia will lose between 29% and 67% of their total mass by 2100.

The new study investigated how the amount of water flowing through the river has changed as a result of melting glaciers and snow and changes in rainfall. This is the first study to look at the entire mountain range and its river and zoomed in to examine how each individual section of these rivers was impacted. 

“Increased river discharge offers short term benefits such as more water for hydropower and agriculture, but it also signals sediment increase and glacier loss,” said  Jonathan Flores, an engineer at the University of Massachusetts and lead author on the study. “If these glaciers continue to shrink, their meltwater contribution to river systems will decline, which will then threaten long term water availability for the downstream.”

The study was published today in AGU Advances, which publishes high-impact, open-access research and commentary across the Earth and space sciences. The research measured more rivers than previous studies and divided them into 8-kilometer (5 mile) segments, which provided more detailed and tailored results.

Researchers found that 10% of rivers had seen an increase in river discharge, or the amount of water moving through the river, during the study period from 2004 to 2019. On average, these rivers saw the discharge rate increase of 8% per year. Sections of larger rivers that have more than 1000 cubed meters (265,000 gallons) of water moving through them per second, such as the Yangtze, had an average increase of over 2% per year, or an extra 5,300 gallons per second. Increases upstream may not correlate to increasing discharge further downstream, which is the case for many of the measured rivers.

The results show a double-edged sword. An increase in water can help with agriculture, electricity and general water usage, but an increase in water discharge directly correlates to an increase in stream power, or how much sediment like sand, silt and gravel is being moved through the river.

Sediment is natural in waterways, but an increase in sediment can come with consequences. Increased sediment can slow down machinery inside hydropower machinery, accumulate inside dams meant to hold water for the dry seasons, and damage river ecosystems with sensitive wildlife.

“The natural aquatic habitat can be altered by this increasing trend and the ecosystems that were previously stable can be altered and changed,” said Flores. Rivers in the western part of High Mountain Asia are fed by glaciers where rivers in the east are mostly filled through rain. As a result, it was primarily the rivers in the west that saw an increase in discharge because climate change is increasing the speed of melting glaciers.

They used over one million pictures from Landsat and PlanetScope satellites to track the changes of the rivers while confirming their estimates through water gauge measurements from various sites across the region.

The information they collected is open source for anyone to use. As plans are made for the construction of new dams or hydropower plants, this information could be used to increase how much water the plants could intake, meaning higher water storage or increased electrical capacity.

“Most of the water infrastructure like dams are designed based on historical data,” said Flores. “They can see that in this study we found that there are increasing trends in the data, so that can be a factor in their decision and planning and optimizing the design.”

Of the 1600 dams or planned dams measured in the study, 8% saw an increase in stream power, meaning more sediment moving through the dams. Flores said the increase in sediment could lead to higher stress being put on the machinery as it would need to move not just the water, but all the sand and dirt it begins to accumulate. Additionally, dams used to store water during the dry season could fill up with sediment and limit their capacity.

“When we tried to have a field visit in Nepal, we were able to visit these communities and hydropower plants and infrastructure, and we found that these are very important to them,” Flores said. “Most of the communities are reliant on hydropower electricity in this region.”

Flores said he hopes the open-source information can be used by local communities to better plan their water resource management for coming years.

Notes for journalists: 

This study is published in AGU Advances, an open-access AGU journal. View and download a pdf of the study here. Neither this press release nor the study is under embargo. 

Paper title: 

“Accelerating river discharge in High Mountain Asia”

Authors: 

  • Jonathan Flores (corresponding author), Department of Civil and Environmental Engineering, University of Massachusetts, Amherst, Massachusetts, USA
  • C. J. Gleason, University of Massachusetts, Amherst, Massachusetts, USA
  • C. Brown, University of Massachusetts, Amherst, Massachusetts, USA
  • N. Vergopolan, Rice University, Houston, Texas, USA
  • M. M. Lummus, University of Pennsylvania, Philadelphia, Pennsylvania
  • L. A. Stearns, University of Pennsylvania, Philadelphia, Pennsylvania
  • D. Li, Peking University, Beijing, China
  • L. C. Andrews, NASA Goddard Space Flight Center, Globel Modeling and Assimilation Office, Greenbelt, Maryland, USA
  • D. Basnyat, Nepal Development Research Institute, Patan, Nepal
  • C. B. Brinkerhoff, Yale School of the Environment, Yale Institute for Biospheric Studies, Yale University, New Haven, Connecticut, USA
  • R. Ducusin, York University, Toronto, Ontario, CAN
  • D. Feng, University of Cincinnati, Cincinnati, Ohio, USA
  • E. Friedmann, University of Massachusetts, Amherst, Massachusetts, USA
  • X. He, University of Massachusetts, Amherst, Massachusetts, USA
  • M. Girotto, University of California, Berkeley, California, USA
  • S. V. Kumar, NASA Goddard Space Flight Center, Globel Modeling and Assimilation Office, Greenbelt, Maryland, USA
  • R. B. Lammers, University of New Hampshire, Durham, New Hampshire, USA
  • G. Lamsal, Nepal Development Research Institute, Patan, Nepal
  • F. Z. Maina, NASA Goddard Space Flight Center, Globel Modeling and Assimilation Office, Greenbelt, Maryland, USA
  • A. A. Proussevitch, University of New Hampshire, Durham, New Hampshire, USA
  • A. Richey, Washington State University, Pullman, Washington, USA
  • E. Shevliakova, NOAA Geophysical Fluid Dynamics Laboratory, Princeton, New Jersey, USA
  • D. Subedi, Nepal Development Research Institute, Patan, Nepal
  • J. Wang, University of Illinois, Kansas State University, Champaign, Illinois, USA

AGU (www.agu.org) is a global community supporting more than half a million advocates and professionals in Earth and space sciences. Through broad and inclusive partnerships, AGU aims to advance discovery and solution science that accelerate knowledge and create solutions that are ethical, unbiased and respectful of communities and their values. Our programs include serving as a scholarly publisher, convening virtual and in-person events and providing career support. We live our values in everything we do, such as our net zero energy renovated building in Washington, D.C. and our Ethics and Equity Center, which fosters a diverse and inclusive geoscience community to ensure responsible conduct. 

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‘Revolutionary’ seafloor fiber sensing reveals how falling ice drives glacial retreat in Greenland




University of Washington
Fiber optic cable load IMG1 

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Dominik Gräff, a University of Washington postdoctoral researcher in Earth and space sciences (pictured in the center), and two crew members load the fiber optic cable, spooled around a large drum, onto the back of the research vessel Adolf Jensen.

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Credit: Manuela Köpfli/University of Washington






As glaciers melt, huge chunks of ice break free and splash into the sea, generating tsunami-size waves and leaving behind a powerful wake as they drift away. This process, called calving, is important for researchers to understand. But the front of a glacier is a dangerous place for data collection.  

To solve this problem, a team of researchers from the University of Washington and collaborating institutions used a fiber-optic cable to capture calving dynamics across the fjord of the Eqalorutsit Kangilliit Sermiat glacier in South Greenland. Data collected from the cable allowed them to document — without getting too close — one of the key processes that is accelerating the rate of glacial mass loss and in turn, threatening the stability of ice sheets, with consequences for global ocean currents and local ecosystems.  

“We took the fiber to a glacier, and we measured this crazy calving multiplier effect that we never could have seen with simpler technology,” said co-author Brad Lipovsky, a UW assistant professor in Earth and space sciences. “It’s the kind of thing we’ve just never been able to quantify before.”   

The data provides, for the first time, a deeper look at the relationship between ice and the water it collapses into, from surface waves to disturbances within the water column. 

Their findings were published in Nature on Aug. 13.  

The Greenland ice sheet — a frozen cap about three times bigger than Texas — is shrinking. Scientists have documented its retreat for the past 27 years as they scramble to understand the consequences of continued mass loss. If the Greenland ice sheet were to melt, it would release enough water to raise global sea levels by about 25 feet, inundating coastlines and displacing millions of people.   

Researchers also speculate that ice loss is weakening a global current system that controls the climate and nutrient distribution by circulating water between northern and southern regions, called the Atlantic meridional overturning circulation.   

“Our whole Earth system depends, at least in part, on these ice sheets,” said lead author Dominik Gräff, a postdoctoral researcher in Earth and space sciences. “It’s a fragile system, and if you disturb it even just a little bit, it could collapse. We need to understand the turning points, and this requires deep, process-based knowledge of glacial mass loss.”   

For the researchers, that meant taking a field trip to South Greenland — where the Greenland ice sheet meets the Atlantic Ocean — to deploy the fiber-optic cable. In the past decade, researchers have been exploring how these cables can be used for remote data collection through technology called Distributed Acoustic Sensing, or DAS, that records ground motion based on cable strain. Before this study, no one had attempted to record glacial calving with a submarine DAS cable.  

“We didn’t know if this was going to work,” said Lipovsky. “But now we have data to support something that was just an idea before.”  

Researchers dropped a 10-kilometer cable from a boat near the mouth of the glacier. They connected it to a small receiver and collected ground motion data and temperature readings along the length of the cable for three weeks.   

The backscatter pattern from photons passing through the cable gave researchers a window beneath the surface. They were able to make nuanced observations about the enormous chunks of ice speeding past their boat. Some of which, said Lipovsky, were the size of a football stadium and humming along at 15 to 20 miles per hour.     

Glaciers are huge, and most of their mass sits below the surface of the water, where ice melts faster. As warm water eats away at the base, the glacier becomes top-heavy. During a calving event, chunks of the overhanging portion break off, forming icebergs. Calving can be gradual, but every so often, the glacier heaves a colossal chunk of ice seaward. The researchers witnessed a large event every few hours while conducting their field work.

“When icebergs break off, they excite all sorts of waves,” said Gräff.   

Following the initial impact, surface waves — called calving-induced tsunamis — surged through the fjord. This stirs the upper water column, which is stratified. Seawater is warmer and heavier than glacial melt and thus settles at the bottom. But long after the splash, when the surface had stilled, researchers observed other waves, called internal gravity waves, propagating between density layers.  

Although these underwater waves were not visible from the surface, the researchers recorded internal waves as tall as skyscrapers rocking the fjord. The slower, more sustained motion created by these waves prolonged water mixing, bringing a steady supply of warmer water to the surface while driving cold water down to the fjord bottom.   

Gräff compared this process to ice cubes melting in a warm drink. If you don’t stir the drink, a cool layer of water forms around the ice cube, insulating it from the warmer liquid. But if you stir, that layer is disrupted, and the ice melts much faster. In the fjord, researchers hypothesized that waves, from calving, were disrupting the glacier’s boundary layer and speeding up underwater melt.   

Researchers also observed disruptive internal gravity waves emanating from the icebergs as they moved across the fjord. This type of wave is not new, but documenting them at this scale is. Previous work relied on site specific measurements from ocean bottom sensors, which capture just a snapshot of the fjord, and temperature readings from vertical thermometers. The data could help improve forecasting models and support early warning systems for calving-induced tsunamis.  

“There is a fiber-sensing revolution going on right now,” said Lipovsky. “It’s become much more accessible in the past decade, and we can use this technology in these amazing settings.”    

Other authors include Manuela Köpfli, a UW graduate student in Earth and space science; Ethan F. Williams a UW postdoctoral researcher in Earth and space science, Andreas Vieli, Armin Dachauer, Andrea Knieb-WalterDiego Wasser, Ethan Welty of University of Zurich, Daniel FarinottiEnrico van der Loo, Raphael Moser, Fabian Walter of ETH Zurich, Jean-Paul Ampuero, Daniel Mata Flores, Diego Mercerat and Anthony Sladen of the Université Côte d’Azur, Anke Dannowski and Heidrun Kopp of GEOMAR | Helmholtz Centre for Ocean Research Kiel, Rebecca Jackson of Tufts University, Julia Schmale, of École Polytechnique Fédérale de Lausanne, Eric Berg of Stanford University, and Selina Wetter of the Université Paris Cité 

This research was funded by the U.S. National Science Foundation, the University of Washington's FiberLab, the Murdock Charitable Trust, the Swiss Polar Institute, the University of Zurich, ETH Zurich, and the German Research Center for Geosciences GFZ. 

For more information, contact Dominik Gräff at graeffd@uw.edu.

Journal

DOI

Article Title

Article Publication Date

Falling ice drives glacial retreat in Greenland




University of Zurich

Iceberg calving 

image: 

Blick auf den Fjord und die drei Kilometer breite Kalbungsfront des Eqalorutsit Kangilliit Sermiat in Südgrönland. Das Glasfaserkabel wurde einige hundert Meter von der Eiswand entfernt durch das 300 Meter tiefe Wasser auf dem Meeresgrund verlegt. Im Vordergrund ist das Radargerät der UZH zu sehen, das Kalbungsereignisse und Eisbewegungen misst, um die Daten des Glasfaserkabels zu interpretieren.

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Credit: Andreas Vieli






Iceberg calving occurs when masses of ice break away from the edge of glaciers and crash into the ocean. This process is one of the major drivers of the rapid mass loss currently affecting the Greenland ice sheet. An international research team led by the University of Zurich (UZH) and the University of Washington (UW) has now used fiber-optic technology to measure for the first time how the impact of falling ice and its subsequent drift is driving the mixing of glacial melt with warmer subsurface seawater.

“The warmer water increases seawater-induced melt erosion and eats away at the base of the vertical wall of ice at the glacier’s edge. This, in turn, amplifies glacier calving and the associated mass loss from ice sheets,” says Andreas Vieli, a professor at UZH’s Department of Geography and co-author of the study. Vieli heads the Cryosphere cluster, one of six clusters in the interdisciplinary GreenFjord project in southern Greenland, supported by the Swiss Polar Institute. These new insights into the dynamics of glacier ice and seawater are featured on the cover of the latest issue of Nature.

Wave measurements using fiber-optic cable on seafloorAs part of the GreenFjord project, UZH and UW were joined by other Swiss institutions to conduct an extensive field study into the dynamics of glacier calving. The researchers deployed a ten-kilometer-long fiber-optic cable onto the seafloor across the fjord of the Eqalorutsit Kangilliit Sermiat glacier. This large, fast-flowing glacier in South Greenland releases around 3.6 km3 of ice into the sea every year – almost three times the volume of the Rhône glacier at the Furka mountain pass in Switzerland.

The researchers used a technology called Distributed Acoustic Sensing (DAS), which detects ground motion by monitoring cable strain caused by crevasses forming in the ice, falling ice blocks, ocean waves or changes in temperature. “This enables us to measure the many different types of waves that are generated after icebergs break off,” says lead author Dominik Gräff, a UW postdoctoral researcher affiliated with ETH Zurich.

Underwater waves amplify glacier melt and erosionFollowing the initial impact, surface waves, known as calving-induced tsunamis, surge through the fjord, initially mixing the upper layers of water. As seawater in Greenland’s fjords is warmer and denser than glacial meltwater, it sinks to the bottom.

But the researchers also observed other waves propagating between density layers long after the splash, when the surface had stilled. These underwater waves, which can be as tall as skyscrapers, are not visible from the surface but prolong water mixing, bringing a steady supply of warmer water to the surface. This process increases melting and erosion at the glacier’s edge and drives ice calving. “The fiber-optic cable allowed us to measure this incredible calving multiplier effect, which wasn’t possible before,” says Gräff. The data collected will help document iceberg calving processes and improve our understanding of the accelerating loss of ice sheets.

A fragile and threatened system

Scientists have long recognized the significance of seawater and calving dynamics. However, measuring the relevant processes on site presents considerable challenges, since the vast number of icebergs along the fjords poses a constant risk from falling chunks of ice. In addition, conventional remote sensing methods based on satellites cannot penetrate below the water’s surface, where interactions between glaciers and seawater take place. “Our previous measurements have often merely scratched the surface, so a new approach was needed,” says Andreas Vieli.

The Greenland ice sheet is a vast body of ice that covers an area roughly 40 times the size of Switzerland. If it were to melt, it would release enough water to raise global sea levels by approximately seven meters. The substantial meltwater volumes released by retreating glaciers can weaken ocean currents such as the Gulf Stream, with far-reaching consequences for Europe’s climate. In addition, the loss of these calving glaciers also affects the local ecosystem of Greenland’s fjords. “Our entire Earth system depends, at least in part, on these ice sheets. It’s a fragile system that could collapse if temperatures rise too high,” warns Dominik Gräff.

Literature

Dominik Gräff et al. Calving-driven fjord dynamics resolved by seafloor fibre sensing. Nature. 13 August 2025 DOI: 10.1038/s41586-025-09347-7

GreenFjord project

Prof. Dr. Julia Schmale (GreenFjord project leader)

Extreme Environments Research Laboratory

Institute for Environmental Engineering

École Polytechnique Fédérale de Lausanne (EPFL)

+41 21 695 82 69

julia.schmale@epfl.ch

https://greenfjord-project.ch

  

Researcher Dominik Gräff (left) and a crew member on their way to shore in a Zodiac boat.  (Image: Julia Schmale, EPFL) 

 

Cornell researchers explore alternatives to harmful insecticide




Cornell University




ITHACA, N.Y. - Cornell University research offers a number of alternatives to neonicotinoids (neonics) that might work for farmers who grow large-seeded vegetable crops such as snap bean, dry bean and sweet corn. This class of insecticides has devastating ecological impacts, especially to pollinators, beneficial insects and aquatic invertebrates.

 

“We wanted to find other options for growers to protect their vegetable crops from major pests. The impetus was to identify new products including those in the registration pipeline,” said Brian Nault, professor of entomology. “My program has shifted in recent years and has focused on this major issue.”

 

The task has not been easy, he added. “Insecticides kill insects, so it’s a tall order to find those that kill the pests but have minimal effects on pollinators and other beneficial insects.”

 

The race to find alternatives to neonicotinoids is urgent, Nault said, because the Birds and Bees Protection Act in New York state is phasing out the sale, distribution or purchase of certain neonicotinoid-treated corn, soybean or wheat seeds starting in the next few years.

 

Research shows neonics have made U.S. agriculture more harmful to insects, and the Environmental Protection Agency determined that neonics likely jeopardize the continued existence of more than 200 threatened and endangered species.

 

The researchers conducted field studies from 2021 to 2024 across Delaware, Minnesota, New York, Washington and Wisconsin. They compared protection of vegetable crops from seedcorn maggot using standard neonicotinoid seed treatments, thiamethoxam and clothianidin, with non-neonicotinoid alternatives including spinosad, cyantraniliprole, chlorantraniliprole, isocycloseram and tetraniliprole. They also compared the risk of these alternative insecticides to workers, consumers and the environment using the Environmental Impact Quotient (EIQ) developed by Cornell University's Integrated Pest Management Program.

 

They found that cyantraniliprole and spinosad seed treatments in snap bean performed as well and occasionally better than the neonicotinoid standard, thiamethoxam. None of the alternative insecticide seed treatments in dry bean provided consistent and reliable protection against seedcorn maggot compared with neonics. But the big triumph was that five different alternative seed treatments (chlorantraniliprole, cyantraniliprole, isocycloseram, spinosad and tetraniliprole) proved as effective as standard neonics for sweet corn.

 

“Sweet corn is a pretty big crop in New York state,” Nault said. So there is good news about alternatives for sweet corn, less so for dry beans and snap beans, he said. For all of the alternative pesticides, their research shows, supplemental options may be necessary to cover additional pests.

 

“For many vegetable crops, farmers could replace the neonic at planting but may need another pesticide later in the season,” Nault said. Other important factors will need to be considered before adopting non-neonicotinoid alternative seed treatments. For example, many are not yet approved for commercial use on these specific crops, and the cost of these newer products will undoubtedly be more expensive than neonicotinoids.

 

For additional information, read this Cornell Chronicle story.

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