Tuesday, September 02, 2025

The tipping of the last resilient glaciers



When the Soviet Union’s collapse meant no glacier data for decades in Tajikistan



Institute of Science and Technology Austria

Researchers' base camp in central Tajikistan 

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Researchers’ headquarters. Base camp north of Maidakul Lake, close to Kyzylsu Glacier, during the first field visit in June 2021. Northwestern Pamir mountains, central Tajikistan.

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Credit: © Marin Kneib/ISTA





Too little snowfall is now also shaking the foundations of some of the world’s most resilient 'water towers', a new study led by the Pellicciotti group at the Institute of Science and Technology Austria (ISTA) shows. After establishing a monitoring network on a new benchmark glacier in central Tajikistan, the international team of researchers was able to model the entire catchment’s behavior from 1999 to 2023. The results, showing decreasing glacier health, were published in Communications Earth & Environment.

High-mountain Asia has been nicknamed the Third Pole due to its massive meltwater reserves, which are second only to the Arctic and Antarctic polar caps. In Central Asia, the northwestern Pamir Mountains in Tajikistan have been home to some of the last stable or growing glaciers outside the polar regions. However, between the collapse of the Soviet Union and the return of new monitoring networks, this region has also suffered from a dire lack of observational data for decades.

Researchers from Professor Francesca Pellicciotti’s group at the Institute of Science and Technology Austria (ISTA) are contributing to an international effort to address this issue. They teamed up with local researchers in Tajikistan and collaborators in Switzerland, Austria, and France to establish their own climate station on a benchmark catchment and model the glacier’s changes over more than two decades. Now, their first joint publication shows evidence that the glacier likely reached its tipping point in 2018.

“Due to the general lack of data and robust future projections in the region, we can’t tell yet whether this was truly the ‘point of no return’ for Pamir glaciers,” says the study’s first author, Achille Jouberton, a PhD student in the Pellicciotti group at ISTA. “We must keep in mind that this study only considers one specific catchment and extends from 1999 to 2023. However, it is the first study of its kind. Similar efforts will need to address these issues on a larger geographical scale.”

Understanding an anomalous state

Climate change has had a substantial impact on glaciers worldwide. While those in the Alps, Andes, and elsewhere in the world have been melting at a disconcerting rate, some glaciers in the Central Asian Pamir and Karakoram mountains were found to be surprisingly stable, possibly even growing. This unexpected and counterintuitive behavior of the glaciers has been termed the Pamir-Karakoram Anomaly. “Central Asia is a semiarid region that is highly dependent on snow and ice melt for downstream water supply,” says ISTA Professor Pellicciotti. “But we still do not fully understand the causes of this anomalous glacier state.” Are these the last resilient glaciers in the face of climate change?

The team chose to establish their monitoring site on Kyzylsu Glacier in the northwestern Pamir, in central Tajikistan. This climate station is situated at an elevation of just below 3400 meters above sea level in a country where half of the territory rises above 3000 meters. “Kyzylsu is becoming a benchmark monitoring site due to the various observational sites recently established on and around the glacier,” explains Jouberton. There, the researchers aim to start to shed light on the glaciers’ anomalous behavior in the region.

“The challenge is that there is almost no data at all.”

Since setting up their monitoring network at the Kyzylsu catchment in 2021, the team has collected extensive data about snowfall and water resources in the area. Using these observations and climate reanalysis data as inputs to their computational models, they were able to simulate the glacier’s behavior from 1999 to 2023. “We modeled the catchment’s climate, its snowpack, the glacier mass balances, and the water movements,” says Jouberton. “But whichever way we analyzed the model, we saw an important tipping point in 2018 at the latest. Since then, the decreased snowfall has changed the glacier’s behavior and affected its health.”

In fact, the glacier ice melt has increased, compensating for around a third of the lost water resources from reduced precipitation. Therefore, it seems the anomalous phase of the glacier’s relative stability in the face of climate change has reached its end.

The researchers used computational models driven by their critically important, new local observations. However, observational data alone would not have answered all questions, even if dense coverage was provided. “We need models and simulations anyway in our work, from the bottom of the valley to the top of the glacier. Even in Europe and Canada, where the monitoring networks are much more extensive, climate stations remain small, localized points on the map,” says Jouberton. “But the challenge in the Pamir region is that there is almost no data at all.” Therefore, the researchers have to densify the observational mesh. “In light of all these challenges, we are not sure how accurate the input to the model is. But since it performed well against independent observations, we are quite confident about the output. Our work is a first step in the right direction.”

Backpacks loaded with precious equipment

Since establishing the collaboration in 2021, while the Pellicciotti group was located at the Swiss Federal Institute for Forest, Snow and Landscape Research (WSL), the researchers have visited Tajikistan seven times. “We’ve planned field trips every summer with the local research institutes in Dushanbe and hiked with our backpacks loaded with precious equipment to set camp in remote mountains, cut off from the world. Having local scientists as part of the field trip not only favors close collaboration and scientific exchange but also helps us overcome the language barrier while interacting with the local inhabitants who depend on the glaciers,” says Jouberton.

2025 marks a milestone as this summer’s field trip was the last one within the project’s current funding period. Among this year’s goals were updating and automating the monitoring networks to ensure they remain functional for decades to come. By also sharing essential knowledge about the equipment’s maintenance with local inhabitants, they hope to make their work more sustainable and reduce the need for frequent field trips. Up to now, they had to travel to exchange the equipment’s internal batteries, maintain the stations’ functionality, and collect their data using USB sticks.

Considerable local impact

The team’s work relies on close cooperation with the locals. “The shepherds know us. They see us every year and often invite us for lunch. They know where we set up our stations and do their best to ensure that nothing disturbs the measurements,” says Jouberton. The team discusses the data with the locals, shares information, and works in the wilderness amid the local inhabitants, their children, and livestock. Frequently, the locals report events that have happened in the mountains. “It is impressive to hear the locals tell us about things we only saw in satellite data. This gives a real and personal impact to our work.”

The Kyzylsu catchment contributes to the drainage basin of the Amu Darya, one of the major rivers in Central Asia, whose water originates almost entirely from glaciers. The Amu Darya is also a former inflow of the now mostly dried-up Aral Sea. This inland sea has suffered from the ongoing decades-long diversion of its two main inflow rivers, the Amu Darya to the south and the Syr Darya to the northeast, to irrigate cotton fields created in the desert during Soviet times. “But the effects of the glaciers are the strongest in their immediate ecosystems,” says Jouberton. “Even though the Kyzylsu Glacier and likely other Pamir glaciers seem to be melting faster and pumping more water into the system, it is unlikely that they will refill what’s left of the Aral Sea.”

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The present study was conducted by researchers from the Pellicciotti group at the Institute of Science and Technology Austria (ISTA), previously at the Swiss Federal Research Institute WSL, Switzerland, in collaboration with scientists from the Institute of Environmental Engineering, ETH Zurich, Switzerland, the University of Zurich, Department of Geography, Glaciology and Geomorphodynamics Group, Switzerland, the Department of Geosciences, University of Fribourg, Switzerland, the Institut des Géosciences de l’Environnement, Université Grenoble-Alpes, CNRS, IRD, France, the Department of Atmospheric and Cryospheric Sciences, University of Innsbruck, Austria, the Geophysical Institute, University of Alaska Fairbanks, USA, the Center for the Research of Glaciers of the Tajik Academy of Tajikistan, Dushanbe, Tajikistan, and the Mountain Societies Research Institute, University of Central Asia, Dushanbe, Tajikistan.

HKU climate research finds hotspot of tropical storm clusters shifting from Pacific to Atlantic



The University of Hong Kong

GOES-16 satellite image 

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This GOES-16 satellite image from the National Oceanic and Atmospheric Administration (NOAA), taken on September 14, 2020, shows five active tropical systems spinning in the Atlantic basin at one time. From the left: Hurricane Sally in the Gulf of Mexico, Hurricane Paulette east of the Carolinas, the remnants of Tropical Storm Rene in the central Atlantic, and Tropical Storms Teddy and Vicky in the eastern Atlantic. A total of 10 named storms formed in September 2020 — the highest number ever recorded in a single month. Image courtesy of NOAA.

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Credit: NOAA





A new study co-led by Professor Dazhi XI, climatologist from the Department of Earth and Planetary Sciences at The University of Hong Kong (HKU), and Zheng-Hang FU, a PhD student from Fudan University reveals that over the past decades, clustered tropical cyclone—storms that occur in close succession—are becoming less frequent in the Northwestern Pacific, including Hong Kong, Japan, and the Philippines, while becoming more common in the North Atlantic, affecting regions such as the U.S. East Coast and the Caribbean. The study, titled “Shifting Hotspot of Tropical Cyclone Clusters in a Warming Climate,” was recently published in Nature Climate Change.

Tropical cyclones, commonly known as typhoons or hurricanes, do not always strike alone. Sometimes, they form in clusters—two or more storms developing simultaneously within the same ocean basin. This phenomenon is not rare—historically, only 40% of tropical cyclones appeared alone. For example, in September 2024, typhoon Bebinca and tropical storm Pulasan made landfall in Shanghai, within three days of each other, disrupting the city’s infrastructure before recovery efforts could fully begin.

These cluster events can cause disproportionate damage, as affected regions have limited time to recover between successive storms. Therefore, understanding the mechanisms and trends behind these events is essential for coastal risk management.

“We wanted to understand whether these clustering patterns are simply coincidental or whether something deeper is going on,” said Professor Dazhi Xi, climatologist at HKU Earth and Planetary Sciences and co-author of the study.

“We developed a probabilistic framework to investigate whether the observed changes in cyclone clusters could be explained by random factors alone. If clusters simply form by chance, their occurrence should depend only on how often storms form, how long they last, and when they occur during the season. So, we built a model based on these three factors to simulate storm clusters over the recent decade, giving us a baseline to compare against actual observations.” 

Key Findings from the Study

  • Clustered storms are increasing in the North Atlantic but declining in the Northwestern Pacific.
  • Using a probabilistic model, the research suggests that changes in storm frequency are the primary driver behind the shifting of cluster hotspots. Other factors, such as storm duration and timing, play only secondary roles.
  • However, in some years, the model significantly underestimates the actual number of clustered storms, indicating that not all clusters form by chance.
  • These exceptions are linked to synoptic-scale waves—a series of train-like atmospheric disturbances that actively increase the chance of tropical cyclone cluster formation.
  • The shift in clustering patterns appears to be driven by a La Niña–like global warming pattern, where the Eastern Pacific is warming more slowly than the Western Pacific. This warming pattern not only modulates storm frequency but also affects the strength of the synoptic-scale waves, further contributing to the relocation of cyclone clusters from the Pacific to the Atlantic.


Action on Storm-Ready Infrastructure

The research implies a growing threat of back-to-back tropical cyclones along North Atlantic coastlines. To address these growing risks, both coastal infrastructure and emergency response systems must be strengthened. This includes reinforcing the drainage system, improving the resilience of the power grid, and enhancing the reliability of water supply networks to withstand the hazards of multiple storms. Emergency response teams must also be better prepared to manage multiple storm attacks in quick succession.

The Journal paper can be accessed from here: https://www.nature.com/articles/s41558-025-02397-9

For media enquiries, please contact HKU Faculty of Science (tel: 852-3917 4948/ 3917 5286 ; email: caseyto@hku.hk / cindycst@hku.hk ).

Images download and captions: https://www.scifac.hku.hk/press

 

The ocean carbon sink is ailing





ETH Zurich





The world’s oceans act as an important sink for carbon dioxide (CO₂). To date, they have absorbed around a quarter of human-induced CO₂ emissions from the atmosphere, thereby stabilising the global climate system. Without this sink, the CO₂ concentration in the atmosphere would be much higher and global warming would have already significantly exceeded the 1.5-degree warming limit. At the same time, the ocean absorbs around 90 percent of the additional heat from the atmosphere. 

In the year 2023, the surface temperatures of the world’s ocean rose sharply, topping record levels in various regions. The tropical Pacific was very warm due to a strong El Niño event, which reverses the currents in this ocean region so that warm surface water accumulates off the coast of South America and colder water no longer rises from deeper layers. At the same time, the ocean outside the tropics also warmed up exceptionally strongly, especially the North Atlantic.

“This sudden warming of the ocean to new record temperatures is challenging for climate research – because to date it was unclear how the marine carbon sink would respond,” says Nicolas Gruber, Professor of Environmental Physics at ETH Zurich. 

An international research team has now investigated for the first time, based on oceanic CO2 measurements from a global observation network, whether and how the extreme temperatures recorded two years ago impacted this sink. The team was headed by ETH biogeochemist Jens Daniel Müller, who was a postdoctoral researcher in Gruber’s group until recently.

In a study published in the journal Nature Climate Change, the researchers show that in 2023, the global ocean absorbed almost one billion tonnes or around ten percent less CO₂ than anticipated based on previous years. This corresponds to about half of the EU’s total CO₂ emissions or more than 20 times those of Switzerland. “This is not good news,” Gruber notes, “but the decline is smaller than feared.”

Warm water dissolves less CO₂

In fact, the decline did not really surprise the researchers. By way of an everyday phenomenon, Müller explains exactly why: “When a glass of carbonated water warms up in the sun, dissolved CO₂ escapes into the air as a gas.” And the same phenomenon happens in the sea. 

The fact that the global ocean absorbed less CO2 in the record-hot year of 2023 was mainly due to the high sea surface temperatures in the extratropical regions of the northern hemisphere, especially in the North Atlantic. “The high temperatures reduced the solubility of CO2, resulting in abnormal CO2 outgassing and reducing the strength of the ocean carbon sink,” as Müller outlines. 

Whether the ocean absorbs or releases CO₂, however, does not depend solely on temperature. If we consider only the reduced CO₂ solubility, the outgassing as a result of the high temperatures in 2023 should have been more than ten times greater – this would have caused the global marine carbon sink to collapse almost completely. 

The study, however, shows that the sink decreased only moderately. According to the researchers, this is due to physical and biological processes in the ocean that counteract CO₂ outgassing and support the sink’s strength. These processes reduce the concentration of dissolved inorganic carbon (DIC) in the surface layers. 

Compensating forces stabilising the sink

In 2023, three physical and biological processes kept DIC low in the near-surface layers. First, CO2 itself escaped, while secondly, a more stable stratification of the water column prevented CO2-rich water from rising from the deeper layers to the surface. And thirdly, the biological pump continuously transported organic carbon into the depths of the ocean: the biological pump is the process by which photosynthetic organisms in the light-flooded layers absorb CO₂ and grow, subsequently die and sink to depths. 

These three compensating forces – the escape of CO2, the stratification of the water column and the biological pump – stabilised the carbon sink. “Consequently, the ocean’s response to the extreme temperatures of 2023 can be understood as the result of a permanent tug-of-war between temperature-induced outgassing and the concurrent depletion of dissolved CO2,” as Gruber states.

El Niño effect overlaid

The researchers explain the influence of the 2023 El Niño on the marine carbon sink in a similar manner: during El Niño years, the circulation in the tropical Pacific weakens, preventing cold, CO2-rich water from rising to the surface. As a result, the tropical eastern Pacific, which in normal years releases very large amounts of CO₂ into the atmosphere, emits essentially no CO₂ during El Niño years. Consequently, El Niño tends to enhance the global sink strength of the ocean – in spite of the strong warming. 

This was also the case in 2023. “The strong warming of the extratropical ocean, however, has negated the El Niño effect in the tropical Pacific,” Müller concludes. In fact, the temperature-driven CO₂ outgassing was so strong, especially in the North Atlantic, that it cancelled out the CO₂ uptake in the tropics. The net result in the El Niño year of 2023 was a reduction of the marine carbon sink.

In conducting their study, the researchers focused on the global ocean (excluding the Arctic Ocean and the southernmost parts of the Southern Ocean). They relied on CO₂ observations from research vessels, cargo ships and measuring buoys, combined with satellite data and machine learning to establish global maps of the surface CO2 levels. This enabled them to calculate the CO₂ fluxes between water and air at the sea surface. 

The future of the marine sink remains uncertain

The study is one of the first to draw on actual observations as a foundation for insights into the behaviour of a warming ocean. “We cannot yet say with certainty, however, how this important carbon sink will develop in the future,” Müller notes.

One thing is clear: since the record-high temperatures of the year 2023, the world’s ocean has hardly cooled down and the earth continues to warm up. Heat waves are becoming more frequent and more intense. “It is unclear, however, as to whether the compensating mechanisms will remain effective over the long term and limit temperature-driven outgassing,” Gruber points out. 

The two researchers concede that the marine carbon sink could absorb less CO₂ in the future. “For the time being, however, the global ocean is still absorbing a great deal of CO₂ – fortunately,” as Gruber states in conclusion.

References

Müller JD, Gruber N, Schneuwly A, Bakker DC, Gehlen M, Gregor L, Hauck J, Landschützer P, McKinley GA: Unexpected decline of the ocean carbon sink under record-high sea surface temperatures in 2023. Nature Climate Change, 2 September 2025, doi: 10.1038/s41558-025-02380-4

For the first time in 40 years, Panama’s deep and cold ocean waters failed to emerge, possibly affecting fisheries and coral health




Smithsonian Tropical Research Institute
Fish school 

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Upwelling events support highly productive fisheries and help protect coral reefs from thermal stress.

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Credit: Natasha Hinojosa





During the dry season in Central America (generally between December and April), northern trade winds generate upwelling events in the ocean waters of the Gulf of Panama. Upwelling is a process that allows cold, nutrient-rich waters from the depths of the ocean to rise to the surface. This dynamic supports highly productive fisheries and helps protect coral reefs from thermal stress. Thanks to this movement of water, the sea along Panama’s Pacific beaches remains cooler during the "summer" vacation season.

Scientists from the Smithsonian Tropical Research Institute (STRI) have studied this phenomenon and their records show that this seasonal upwelling, which occurs from January to April, has been a consistent and predictable feature of the gulf for at least 40 years. However, researchers recently recorded that in 2025, this vital oceanographic process did not occur for the first time. As a result, the typical drops in temperature and spikes in productivity during this time of year were diminished. In the recently published article in the journal PNAS, scientists suggest that a significant reduction in wind patterns was the cause of this unprecedented event, revealing how climate disruption can quickly alter fundamental oceanic processes that have sustained coastal fishing communities for thousands of years. Still, further research is needed to determine a more precise cause and its potential consequences for fisheries.

This finding highlights the growing vulnerability of tropical upwelling systems, which, despite their enormous ecological and socioeconomic importance, remain poorly monitored. It also underscores the urgency of strengthening ocean-climate observation and prediction capabilities in the planet’s tropical regions.

This result marks one of the first major outcomes of the collaboration between the S/Y Eugen Seibold research vessel from the Max Planck Institute and STRI.

Reference: O’Dea, A., Sellers, A. J., Pérez-Medina, C., Pardo Díaz, J., Guzmán Bloise, A., Pöhlker, C., Chiliński, M. T., Aardema, H. M., Cybulski, J. D., Heins, L., Paton, S. R., Slagter, H. A., Schiebel, R., & Haug, G. H. 2025. Unprecedented suppression of Panama's Pacific upwelling in 2025. Proceedings of the National Academy of Sciences: Issue: Vol. 122, Iss. 0). DOI: 10.1073/pnas.2512056122

 

About the Smithsonian Tropical Research Institute

Headquartered in Panama City, Panama, STRI is a unit of the Smithsonian Institution. Our mission is to understand tropical biodiversity and its importance to human welfare, to train students to conduct research in the tropics and to promote conservation by increasing public awareness of the beauty and importance of tropical ecosystems. Watch our video, and visit our websiteFacebookX and Instagram for updates.

 

Bite by bite: How jaws drove fish evolution



U-M study traces jaw innovation and evolution in a once-mighty group of fish




University of Michigan

Dipterus 

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Whole skeleton of Dipterus, an extinct lungfish from the middle Devonian period. Specimen (UMMP 16140) from the University of Michigan Museum of Paleontology.

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Credit: E.M. Troyer/University of Michigan





ANN ARBOR—If you're reading this sentence, you might have a fish to thank.

Fish were the first animals to evolve jaws. They use their jaws primarily to eat, but also for defense, as tools—such as to burrow or to crack open hard food—and even as a form of parental care: some fish carry eggs or their young in their mouths. Jaws are a trait that scientists think fueled evolution among vertebrates, including us. 

Now, a University of Michigan study has shown that a now rare group of fish called lobe-finned fishes enjoyed an explosion of diversity between about 359-423 million years ago. They were an especially diverse group containing many species with rapidly evolving jaws and new innovations in feeding modes. In contrast, the other major group of fishes at the time, ray-finned fishes, had jaws that evolved much more slowly. 

This is surprising because at some point, several million years later, their evolution stalled out. The most famous of these "living fossils" is likely the coelacanth, once thought to be extinct but discovered to be living in the deep ocean in 1938 by one of the most well-known women in science, Marjorie Courtenay-Latimer. Today, just eight species of lobe-finned fishes are recognized by scientists. By contrast, ray-finned fishes comprise about 33,000 species today and include just about any fish you can think of, from goldfish to bass to seahorses. 

The study, led by U-M postdoctoral researcher Emily Troyer, is published in the journal Current Biology and supported by the National Science Foundation. 

Troyer said the study underscores the importance of looking to ancient fossil records to discover new information about the process of evolution. They didn't expect to see such a disparity in evolutionary might between lobe-finned fishes and ray-finned fishes—something that wouldn't have been known if not for the fossil record of Silurian and Devonian fish.

"When you're looking at evolution, you can learn so much from looking at the past," Troyer said. "Without the fossil record, we would have no idea of this inverted role reversal."

The age of fishes

While scientists have long suspected the role of jaws in vertebrate evolution, there was little work that compared jaw evolution among early fishes. The study authors examined 3D models from CT scan data of 86 different species of fishes from the Silurian and Devonian periods, beginning about 443 million years ago—before even trees existed. They found that the lobe-finned fishes, lungfish and coelacanth, in particular, displayed the fastest rates of change and the most innovation in jaw shape and function. 

"This is a really striking result, primarily because lungfish and coelacanths today are represented by only eight living species, with not much jaw diversity going on. However, if we look back in time 400 or so million years, we see this striking inversion. During the Devonian, we have a lot more species and a lot more innovation within their jaws," Troyer said. 

To determine this, the research team digitally mapped each 3D model to examine both the form of the jaw and the function by determining the mechanical advantage of the jaw, or how much force the fish could exert when they bit down.

"Essentially, the higher the mechanical advantage of the jaw, the stronger the bite force," Troyer said. 

The research team found that the shape of lungfish jaws really took off in the early Devonian period. Their jaws grew big and thick, with heavy muscle. This likely gave them the ability to eat hard-shelled prey such as early clams and crustaceans. 

"With their really hefty jaws, they were able to eat really hard food," Troyer said. "We think these new feeding strategies might be causing jaws to need to be shaped like this, and that some of these major innovations are associated with their ecosystems during this time."

Rafael Rivero-Vega, co-first author and recent U-M doctoral graduate, collected CT scan data and visited museums to create additional 3D scans of nearly every available, complete lobe-finned fish jaw fossil for his dissertation. He then mapped important characteristics of the jaws in order to test for "adaptive radiation," or the rapid diversification of animals due to changes in their environment.

Rivero-Vega was struck by the research's revelation that each fish group was experiencing "a unique evolutionary moment in their ancient past."

"Some fishes were diversifying their jaws rapidly in shape and size, only later to stay essentially unchanged once they filled a specialized niche, others had similar characteristics but a wider variety of shapes and sizes, and yet others had similar form but wouldn't change until after they had already transitioned onto land," he said. 

"It's a great example of how innovations in shape, form and function can be explored by different fish groups at their own pace as long as they experience the appropriate evolutionary pressures. And all of this happened hundreds of millions of years before the dinosaurs. Fishes are awesome."