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Inclusion, Diversity, Equity, and Accessibility: Excellent IDEA! 

Wed, 02/18/2026 - 16:07
Editors’ Highlights are summaries of recent papers by AGU’s journal editors. Source: AGU Advances

Inclusion, diversity, equity, and accessibility (IDEA) are recognized as central ethical commitments that strengthen science and expand its impact. However, their contribution to support continued innovation and the factual barriers and enablers are under-documented.

A new study from Naji and Reyes et al. [2026] addresses this gap. The authors conducted semi-structured interviews with underrepresented and underserved Earth observation professionals and identified challenges and support they received during their career. Through these conversations, they identify barriers and enablers and discuss solutions. The authors present interesting quotes from the interviews that excellently convey the feelings and discouragement caused by the barriers and the enthusiasm and scientific benefit stimulated by successful enablers. The article provides an illuminating perspective on the real value of IDEA for the benefit of science and humanity.

Citation: Naji, N., Reyes, S. R., Crowley, M. A., Schenkein, S. F., González, M., Siwe, R., et al. (2026). Global perspectives on barriers and enablers to inclusion, diversity, equity, and accessibility (IDEA) in the field of Earth observation. AGU Advances, 7, e2025AV001858. https://doi.org/10.1029/2025AV001858

—Alberto Montanari, Editor-in-Chief, AGU Advances

Text © 2026. The authors. CC BY-NC-ND 3.0
Except where otherwise noted, images are subject to copyright. Any reuse without express permission from the copyright owner is prohibited.

The Olympics Just Saw Its First “Forever Chemical” Disqualifications

Wed, 02/18/2026 - 13:57

This story was originally published by Grist. Sign up for Grist’s weekly newsletter here.

Heading into the Milan-Cortina 2026 Olympics, skiers and snowboarders were already adjusting to a ban on fluorinated waxes long prized for making their equipment faster. Last week, the Winter Games saw their first enforcement of that rule, which is aimed at protecting public health and the environment.

South Korean cross-country skiers Han Dasom and Lee Eui-jin were disqualified from the women’s sprint event on 10 February. That came one day after Japanese snowboarder Shiba Masaki was disqualified from the men’s parallel giant slalom. In all three cases, routine testing found banned compounds on their equipment.

The so-called “fluoro” waxes provide a “really ridiculous speed advantage.”

For decades, elite snow sports athletes have relied on waxes with fluorocarbons that are exceptional at repelling water and dirt. Former U.S. cross-country racer Nathan Schultz told Grist the so-called “fluoro” waxes provide a “really ridiculous speed advantage,” especially in warmer conditions like those experienced at these Games.

But these waxes also contained PFAS, short for per- and polyfluoroalkyl substances. This class of 15,000 so-called “forever chemicals” are notorious for never breaking down. Studies have linked exposure to PFAS to thyroid disease, developmental problems, and cancer, and research has found elevated levels in ski technicians who regularly handled the waxes. PFAS have also been detected in soil and water near ski venues, including wells drawing from aquifers in Park City, Utah, suggesting broader environmental contamination.

Amid growing concern over the environmental impacts and the risks to skiers, their technicians, and others, the International Ski and Snowboard Federation, or FIS, called for a ban in 2019. The prohibition took effect in 2023, and applies to all events governed by the federation, including nordic, alpine and freestyle skiing, ski jumping, and snowboarding.

Officials test multiple points on each competitor’s equipment, using a technique known as Fourier transform infrared spectroscopy to detect fluoros. If a given spot on a ski or snowboard turns green, it passes. A red result indicates the presence of the banned substance. Three or more red spots leads to disqualification.

Representatives for the Japan team did respond to comment. A spokesperson for the Korea Ski Association initially told the South Korean news agency Newsis that the organization was “perplexed” by the results. “They tested negative in all previous international competitions with no prior issues,” they said. “We will consult experts from wax and ski manufacturers to investigate whether the issue lies with the wax or skis.”

In an emailed statement, the Korean Olympic Committee told Grist that fluorine was detected in what it believed to be fluorine-free waxes. “The Ski Association has purchased [fluorine]-free wax products, so it will protest,” wrote the spokesperson. The team will also replace the wax and check the skis again after cleaning to “prevent recurrence.”

It is unclear if a protest was ever officially filed or what the outcome was. The Korean team declined to elaborate and FIS did not immediately respond to Grist’s questions. But unlike some infractions, like those related to doping, discipline for unintentional fluoro use generally applies only to the event in question. The Korean athletes competed again Thursday in the 10-km freestyle event, finishing 73rd and 80th.

This time the results stood.

Correction 24 February 2026: An earlier version of this story accidentally referred to fluoride instead of fluorine in one paragraph.

—Tik Root, Grist

This article originally appeared in Grist at https://grist.org/accountability/the-olympics-just-saw-its-first-forever-chemical-disqualifications/.

Grist is a nonprofit, independent media organization dedicated to telling stories of climate solutions and a just future. Learn more at Grist.org.

Liquefaction induced by the 29 March 2025 Mw=7.7 Mandalay earthquake

Wed, 02/18/2026 - 08:26

The Landslide Blog is written by Dave Petley, who is widely recognized as a world leader in the study and management of landslides.

Of all the ground impacts induced by large earthquakes, liquefaction often feels to be the most neglected. The costs can be savage, and the long term implications wide ranging.

In this context, a very interesting paper (Valkaniotis et al. 2026) has been published in the journal Engineering Geology, which documents the liquefaction induced by the 29 March 2025 Mw=7.7 Mandalay earthquake in Myanmar. Given the challenges of fieldwork in this highly contested area, the work has been conducted medium resolution remote sensing.

It is an excellent study that demonstrates that liquefaction was extremely wide-ranging. The authors have documented 18,000 locations in which liquefaction has occurred, with the distribution being controlled by both proximity to the rupture (and not to the epicentre) and by the geology. The presence of thick deposits of Holocene fluvial materials, which occur widely in this area, allowed extensive liquefaction to occur.

One aspect that I found particularly interesting, and highly informative, is the comparison of the utility of satellite images with different resolutions for mapping liquefaction features. In particular, they show that 10 metre resolution Sentinel 2 images are useful for mapping liquefaction. So, I thought I’d take a look at the utility of Planet Labs imagery in this context.

One example that Valkaniotis et al. (2026) provide lies at [22.311, 96.012]. The Planet Labs image below shows this area as of 16 March 2025, a few days before the Mandalay earthquake:-

Satellite image of an area of Myanmar prior to the 2025 Mandalay earthquake. Image copyright Planet Labs, used with permission, collected on 16 March 2025.

And this is the same area on 31 March 2025, three days after the eartuqkae:-

Satellite image of an area of Myanmar after the 2025 Mandalay earthquake. Image copyright Planet Labs, used with permission, collected on 31 March 2025.

And here is a slider to compare the two images:-

Images by Planet Labs.

In the second image, there are hundreds of areas of exposed fluvial deposits (the light coloured patches) that are not present in the first image. These are the areas of liquefaction mapped by Valkaniotis et al. (2026). I think there may also be some locations in which lateral spreads are visible too, but this is less clear.

This is a fascinating finding, which will be very helpful in assessing post-seismic impacts in the future.

The extant of the liquefaction after the 2025 Mandalay earthquake is very interesting. At the end of the day, studies like this provide insight into the response of the ground to large earthquakes, and in turn this is intended to allow us to build resilience to these events. Valkaniotis et al. (2026) conclude their article as follows:-

“The 2025 Mandalay event serves as a reminder that liquefaction remains one of the most devastating secondary hazards associated with strong earthquakes, especially in densely populated floodplains with complex dynamic fluvial histories. The insights gained from this inventory can not only enhance national seismic resilience efforts in Myanmar but also contribute to the better understanding of liquefaction behavior in large strike-slip earthquakes worldwide.”

Quite.

Reference and acknowledgement

Valkaniotis, S. et al. 2026. Regional-scale inventory and initial analysis of liquefaction triggered by the 2025 Mw 7.7 Mandalay earthquake, Myanmar. Engineering Geology,
363. https://doi.org/10.1016/j.enggeo.2026.108543.

Many thanks to the wonderful people at Planet Labs for providing access to the satellite imagery.

Return to The Landslide Blog homepage Text © 2026. The authors. CC BY-NC-ND 3.0
Except where otherwise noted, images are subject to copyright. Any reuse without express permission from the copyright owner is prohibited.

Models Reveal Imprint of Tectonics and Climate on Alluvial Terraces

Tue, 02/17/2026 - 17:00
Editors’ Highlights are summaries of recent papers by AGU’s journal editors. Source: AGU Advances

River terraces are archives of past environmental and climate change as they form when rivers erode into alluvial plains, leaving behind an elevated flat surface. A sequence of terraces can take tens to hundreds of thousands of years to develop, thus they potentially hold important information over the period of formation. This is the case for the extensive terraces in southern Patagonia.

Through mechanistic models of terrace formation, Ruby et al. [2026] both isolate and combine the key drivers of terrace formation and connect them with the observed terrace shapes. Some terrace shapes were shown to form only under a specific combination of model parameters. This opens a new quantitative way to reveal past tectonic, climatic, and environmental conditions and how these have changed using terraces.  

Citation: Ruby, A., McNab, F., Schildgen, T. F., Wickert, A. D., & Fernandes, V. M. (2026). How sediment supply, sea-level, and glacial isostatic oscillations drive alluvial river long-profile evolution and terrace formation. AGU Advances, 7, e2025AV002035. https://doi.org/10.1029/2025AV002035

—M. Bayani Cardenas, Editor, AGU Advances

Text © 2026. The authors. CC BY-NC-ND 3.0
Except where otherwise noted, images are subject to copyright. Any reuse without express permission from the copyright owner is prohibited.

Restored Peatlands Could Become Carbon Sinks Within Decades

Tue, 02/17/2026 - 14:04

Drained peatlands in Finland can become carbon sinks within just 15 years of restoration, suggests a study published in Restoration Ecology. The findings are a stark contrast to another recent publication that suggests the switch from source to sink can take hundreds of years.

Finland will submit a biodiversity restoration plan to the European Commission this September, and what to do about the country’s 5 million hectares of drained peatland will likely be a hot topic. Teemu Tahvanainen, the author of the new study and a plant ecologist at the University of Eastern Finland (Itä-Suomen Yliopisto), said the upcoming deadline motivated him to add to the conversation.

Moreover, if the country is to one day achieve carbon neutrality, it “cannot neglect those areas,” said peatland ecologist Anke Günther from Universität Rostock, in Germany, who was not involved in the new paper.

Like a Forest with No Air

To understand why pristine peatlands are powerful carbon sinks, imagine a forest without any air between the trees, said Günther. That’s how densely the mosses that make up peat are packed together.

To understand why pristine peatlands are powerful carbon sinks, imagine a forest without any air between the trees, said Günther. That’s how densely the mosses that make up peat are packed together. In some places, peatlands can cover millions of hectares and be meters deep. All told, they contain massive amounts of plant matter and therefore massive amounts of carbon—about a third of the total carbon found on Earth.

Peatlands are waterlogged, which largely prevents the peat from decomposing, but also limits how well trees and other plants can grow. Forestry and agricultural companies, governments, and private landowners often dig trenches to drain off some of the water, making the land available for other uses. But draining peat exposes it to oxygen, which then allows microbes to break it down, releasing carbon dioxide.

Rewetting stops these carbon emissions, but it can also cause others, explained soil scientist Jens Leifeld from the Swiss federal research institute Agroscope, who was not involved in the new study. For example, any trees growing in a drained peatland will die upon rewetting, and their deaths will release carbon dioxide if the trees aren’t harvested. Moreover, rewetting shifts the peatland’s microbial population from aerobic microbes to anaerobic, increasing methane emissions. Studies have produced conflicting answers when asking how restoring peatlands affects carbon emissions. “There was no agreed opinion,” Leifeld said.

Increasing the Resolution

Tahvanainen modeled peatland restoration with greater temporal resolution than in previous studies. Rather than assume that parameters such as methane emissions and decomposition of forest litter will remain the same after rewetting, he predicted how these parameters will vary in the years and decades following.

His take-home message: Restoration can cool the climate in as little as a couple of decades. “I’m saying that it can, which sounds a little bit ambiguous on purpose,” he added. There are many variables his approach can’t account for, he said, such as how climate change will progress and the state of a peatland prior to restoration.

“The results make sense to me in a way that other studies didn’t always.”

“The results make sense to me in a way that other studies didn’t always,” said Günther. It seemed implausible to her that the carbon sequestered through a bit of tree growth would compensate for the vast amount of carbon released from draining a peatland.

But rewetting also has consequences the model doesn’t consider, Leifeld pointed out. For example, rewetting changes the color of the landscape in the winter, taking it from the dark color of a forest to the white color of open snow. Snow reflects more sunlight than trees, which cools Earth.

Only field studies can truly answer the question of how rewetting peatlands will affect their greenhouse gas emissions, said forest ecologist Paavo Ojanen from Natural Resources Institute Finland. These studies are ongoing, but they require following peatlands for years. Until they’re complete, “we don’t have the real measurements,” he said.

For now, Tahvanainen said his work adds nuance to studies reporting that peatland restoration won’t bring climate mitigation in the next hundred years. That’s “just way too strongly put,” he said.

—Saima May Sidik (@saimamay.bsky.social), Science Writer

Citation: Sidik, S. M. (2026), Restored peatlands could become carbon sinks within decades, Eos, 107, https://doi.org/10.1029/2026EO260060. Published on 17 February 2026. Text © 2026. The authors. CC BY-NC-ND 3.0
Except where otherwise noted, images are subject to copyright. Any reuse without express permission from the copyright owner is prohibited.

The massive, developing gully at Pondok Balik in Indonesia

Tue, 02/17/2026 - 08:15

A massive gully has been developing over the last two decades at Pondok Balik. It now covers an area of over 3 hectares.

In Indonesia, a massive and rapidly developing gully is causing considerable concern. Located at Pondok Balik in Central Aceh Regency, Aceh province, this feature has been developing since 2004. Reuters has an excellent gallery of images that is worth a view. There is a really good summary of the history of this gully on The Watchers website too.

There is some nice drone footage of this feature in this SindoNews report on Youtube:-

The location of this very large gully is [4.72374, 96.73117]. This is a Google Earth image of it, captured in June 2025:-

Google Earth image from June 2025 of the massive gully at Pondok Balik in Indonesia.

By comparison, here is an image from February 2015:-

Google Earth image from February 2015 2018 of the massive gully at Pondok Balik in Indonesia.

And here is a slider to compare the two, showing the raid development of the gully:-

Google Earth images

The gully is reportedly developing in loose volcanic materials, which are prone to rapid erosion when disturbed and saturated. In Indonesia, rainfall totals are high.

There are concerns about potential damage to the road seen in the image and to high voltage electricity pylons running through the area. It is proposed to seek to manage the hazard by reinforcing the soil and managing surface and subsurface water. This will not be straightforward or cheap.

Return to The Landslide Blog homepage Text © 2026. The authors. CC BY-NC-ND 3.0
Except where otherwise noted, images are subject to copyright. Any reuse without express permission from the copyright owner is prohibited.

Rocky Shore Erosion Shaped by Multi-Scale Tectonics

Mon, 02/16/2026 - 14:00
Editors’ Highlights are summaries of recent papers by AGU’s journal editors. Source: AGU Advances

Coastal landscapes evolve under the combined influence of wave action, climatic variations, sea‑level change, and tectonic processes. Shoreline evolution is especially important along rocky coasts such as those of the western United States, where it shapes hazards to people and infrastructure and affects exposure to events like tsunamis. In this context, tectonically driven uplift plays a key role over both individual earthquake cycles and longer timescales associated with fault-system and topographic development.

Using a compilation of coastal change metrics and statistical analyses, Lopez and Masteller [2026] identify a tentative link between tectonics and shoreline change. On decadal timescales, uplift can slow coastline retreat, as might be expected. Over many earthquake cycles, however, higher long-term uplift associated with cumulative subduction-zone deformation appears to enhance shoreline retreat. These findings highlight some of the interactions between coastal and solid earth hazards. They also point toward future models that integrate similar constraints to improve our understanding of how earthquakes build topography and how sea level, coastal processes, and tectonics together modulate short‑ and long‑term coastal risk.

Citation: Lopez, C. G., & Masteller, C. C. (2026). Tectonics as a regulator of shoreline retreat and rocky coast evolution across timescales. AGU Advances, 7, e2025AV002065. https://doi.org/10.1029/2025AV002065

—Thorsten Becker, Editor, AGU Advances

Text © 2026. The authors. CC BY-NC-ND 3.0
Except where otherwise noted, images are subject to copyright. Any reuse without express permission from the copyright owner is prohibited.

The 16 June 2024 landslide cluster in Wuping County, Fujian Province, China

Mon, 02/16/2026 - 08:10

Six people were killed when intense rainfall triggered over 6,500 landslides

On 16 June 2024, an extreme rainfall event triggered a dense cluster of landslides and channelised debris flows in Wuping County, Fujian Province, China. This is one of many such events in recent years – anecdotally at least, these events are becoming more common and more severe.

Thus, I very much welcome a paper in the journal Landslides (Liao et al. 2026) that describes this event. The paper is not open access, but this link should allow you to read the full manuscript. The authors highlight the impact of the event – six people were killed (two of whom were never recovered) and hundreds of houses were damaged.

The cluster of landslides centres on the area around [24.94745, 116.29172]. This Planet Labs image, captured on 27 November 2024 after the event, shows some of the landslides triggered:-

Landslides triggered by the 16 June 2024 rainfall event in Wuping County, Fujian Province. Image copyright Planet Labs, used with permission, collected on 27 November 2024.

Note the presence of multiple shallow landslides that have combined to form channelised debris flows. In the centre of the image, by the marker, there is a small reservoir that has been almost entirely infilled by debris from the landslides.

In total, Liao et al. (2026) have mapped 6,526 landslide triggered by the rainfall event. The main initiating rainfall appears to have been a period between 14:00 and 18:00 on 16 June 2024, during which 161 mm was recorded, with a peak intensity of 55 mm per hour. Interestingly, though, the landslide density correlates with rainfall total prior to the main initiating event, rather than to the total rainfall. I wonder whether this indicates that the key parameter (the distribution of peak rainfall intensity, for example) is not being captured in the data?

Very helpfully, Liao et al. (2026) have investigated the mechanism of the landslides in some detail. They find that behaviour differed according to the bedrock lithology. In areas underlain by granite, failure occurred on the interface between the weathered and the unweathered materials, a common situation. In most cases, granitic landslides did not generate channelised debris flows.

On the other hand, in areas underlain by greywacke, failures also occurred in these interface areas, but channelised debris flows were more common. This may be related to the steeper local topography in the greywacke areas.

The paper by Liao et al. (2026) further helps us to understand these clusters of landslides and channelised debris flows, which are proving to be so very destructive. Expect more of these events in the coming months and beyond.

Reference and acknowledgement

Liao, Z., Wu, J., Ma, J. et al. 2026. Characteristics and initiation mechanism of clustered landslides triggered by an extreme rainfall in Wuping County, Fujian Province, ChinaLandslides. https://doi.org/10.1007/s10346-026-02712-1.

Many thanks to the wonderful people at Planet Labs for providing access to the satellite imagery.

Return to The Landslide Blog homepage Text © 2026. The authors. CC BY-NC-ND 3.0
Except where otherwise noted, images are subject to copyright. Any reuse without express permission from the copyright owner is prohibited.

Creating Communities to Help Interdisciplinary Scientists Thrive

Fri, 02/13/2026 - 14:23

Scientists who work across disciplines often dread the question, “What is your field of expertise?” A geographer working in an environmental science department or a social scientist working in an ecology department might find it difficult to articulate how their research, knowledge, and professional networks fit within established fields to colleagues long accustomed to their institutions’ disciplinary expectations and norms.

Most academic structures are still largely organized around relatively narrow disciplinary perspectives, even as the world’s biggest challenges require interdisciplinary solutions.

These moments of discomfort may seem trivial, but they signal a systemic barrier for many scientists and for scientific innovation and problem-solving: Most academic structures are still largely organized around relatively narrow disciplinary perspectives, even as the world’s biggest challenges require interdisciplinary solutions. Addressing natural hazards, biodiversity loss, poverty, and food insecurity simultaneously, for example, depends on scientists collaborating across fields and engaging with partners in other sectors of society.

This issue is not just one of semantics, especially for younger scientists and others who regularly experience its effects. Departments incentivized to select against interdisciplinary science and the absence of clear institutional “homes” for interdisciplinary scientists can create challenges for hiring, evaluation, and promotion. It can also reduce researchers’ sense of professional belonging and increase their feelings of being an imposter, which can affect their ability to contribute and even lead to the loss of scientific talent to other career paths.

Experiences in the field of land system science reflect broader tensions with interdisciplinarity across academic science. Researchers studying land system science, as we do, often find that their work resists neat disciplinary labels. Because this field encompasses the many ways that people and nature interact across Earth’s land surface and how these interactions shape global challenges like biodiversity loss, it can be difficult to describe the field in terms of preexisting academic departments and to identify appropriate funding sources and publication venues.

Here we share experiences navigating tensions that have come with pursuing interdisciplinary science, and we describe how one global interdisciplinary science community, the Global Land Programme (GLP), became a home for our work. Communities such as the GLP not only bring people together but also help create new pathways for turning research into solutions.

Our experiences also suggest practical lessons and actionable steps—especially for early-career scholars—for finding or building supportive communities that span fields and sectors, foster belonging, spark scientific innovation, and connect science to society.

Perceived Deficiencies Versus Demonstrated Proficiencies

As interdisciplinary scientists working across institutions around the world, we’ve seen firsthand the tribulations of bridging silos. Colleagues have often questioned our scientific skills and seen us as outsiders. Some have asked whether our interdisciplinary doctoral degrees “count” as legitimate academic credentials or told us that our research “isn’t science.” Even after establishing our careers, we’ve heard comments such as “Your research doesn’t fit into this science foundation’s remit.”

These critiques can be especially harsh for researchers who already encounter structural barriers within scientific institutions [Liu et al., 2023; Bentley and Garrett, 2023; Woolston, 2021; Carrigan and Wylie, 2023]. Having other people—particularly colleagues around whom you work—define you by perceived deficiencies rather than demonstrated proficiencies is hardly constructive for advancing research into complex challenges.

The scientific literature reveals a disconnect between policy-level acceptance of interdisciplinarity and its practical adoption within academic and research institutions.

National- and international-level policies are increasingly encouraging interdisciplinary research. The European Union, for example, is adopting integrated One Health policy approaches that recognize the interconnections of human, animal, plant, and environmental health and require collaboration across previously distinct disciplines and sectors.

Yet the scientific literature reveals a disconnect between policy-level acceptance of interdisciplinarity and its practical adoption within academic and research institutions, showing that the barriers we’ve faced are widely shared [Andrews et al., 2020; Berkes et al., 2024]. Such obstacles include skepticism from peers, disciplinary prejudice, and funding and department structures that privilege individual, siloed fields. We often must frame research proposals as either social science or natural science, for example, because work that straddles or combines both rarely gets funded.

Unsupportive responses from funding agencies, departments, and colleagues can be demoralizing when added to the background stresses of academia. On the other hand, opportunities to commiserate and trade tips with others can be lifelines. Building communities of interdisciplinary scientists is thus essential, especially for younger scholars who often face the steepest barriers with disciplinary divides [Haider et al., 2018].

Discovering a Global Community

To thrive as an interdisciplinary scientist, one might need to “feel comfortable being uncomfortable” [Marx, 2022]. Achieving such confidence requires mentorship and peer relationships in community. In each of our cases, the GLP provided the professional and emotional support that we greatly needed to feel fulfilled in our careers.

As current or former members of the GLP’s Scientific Steering Committee, we are admittedly biased toward the program’s merits. Nonetheless, having come from different scientific backgrounds, career stages, and geographies, we believe that our collective experiences illustrate how global cross-disciplinary communities can cultivate a supportive culture and amplify the reach and impact of community members’ science.

The GLP emerged in the mid-2000s as a successor to earlier global change research projects focused on land use and land cover, with the goal of bringing together natural and social scientists to study land systems as coupled human-environment systems [de Bremond et al., 2019]. Since then, it has become the reference community for land system science, as well as a home for scientists whose work was falling through disciplinary cracks.

Speakers discuss the GLP’s Science Plan during the 5th Open Science Meeting in 2024. Credit: Ximena Fargas

The organization has been guided by a unifying programmatic framework—articulated in its Science Plan—that incorporates knowledge across disciplines to address pressing global challenges (e.g., biodiversity loss, food insecurity, and poverty). The Science Plan, reevaluated and updated every 5 years, offers a living, collaborative road map of interdisciplinary research priorities—a rarity in academia, where competition for resources and rewards often leaves scientists reluctant to share ideas.

This road map enables researchers to orient their work toward impactful cross-disciplinary research themes and projects. It also outlines the GLP’s core priorities and analytical perspectives, drawing on a range of viewpoints and knowledge, which can guide us to develop shared ideas of what is possible.

The Global Land Programme’s activities have built a culture of mutual respect that values ecological and cultural context and encourages engagement with a broad range of perspectives.

Over time, the collaborative spirit of the GLP’s members has resulted in a rich interdisciplinary community of land system scientists that provides a space for them to reflect on dimensions of academic life other than research (as exemplified, e.g., by this article). Besides offering a supportive professional environment, apart from the skepticism we often encounter in more discipline-specific settings, the GLP’s activities have built a culture of mutual respect that values ecological and cultural context and encourages engagement with a broad range of perspectives.

The GLP has also delivered tangible results for science and society. GLP scientists have advanced modeling of land use going back millennia, contributed to global biodiversity assessments (e.g., in support of the Intergovernmental Science-Policy Platform on Biodiversity and Ecosystem Services), codeveloped new visions for land systems, and made datasets that help track land use changes, such as deforestation, publicly available. The GLP also works to translate land system science into forms relevant for policy and practice. For example, GLP scientists authored “Ten Facts About Land Systems for Sustainability,” a framework intended to inform both research and policy understandings of sustainable land governance.

What began as a space for researchers from across disciplines to connect around land system challenges has become an engine for both scientific innovation and societal relevance. This success adds to our trust in the GLP’s approach to supporting researchers in the often-challenging space of interdisciplinary science.

If You Don’t Have a Community, Make One

For interdisciplinary scientists lacking a home, one path forward is to build a new community of researchers with shared interests.

We were fortunate to find the GLP early in our careers, as not all scientists have access to such communities. But the comfort and confidence that come with belonging should not—and need not—depend on luck. For interdisciplinary scientists lacking a home, one path forward is to build a new community of researchers with shared interests.

Establishing a community of practice within a broader existing organization or research community or even creating a new forum for social networking can provide a space that empowers scientists, including early-career researchers, to navigate interdisciplinary work by connecting with peers who share related interests and challenges.

Experiences from existing communities of practice suggest that these spaces tend to work best when they grow organically [Watkins et al., 2018]. Making it easy for people to join, observe, and participate at their own pace helps create welcoming entry points and encourages such growth. Allowing people to gradually step in, share perspectives, and assume roles and responsibilities strengthens the common dynamic that often develops in these communities, in which a core of more active members is surrounded by a larger group of less active, though still involved, members.

In practice, many scientific communities thrive by communicating through simple and familiar platforms, such as mailing lists, online forums and channels, and recurring online meetups, which lower barriers to participation across institutions and regions. Reaching out to existing societies or research networks—AGU or FLARE (Forests & Livelihoods: Assessment, Research, and Engagement), for example—for guidance on coordination or to help gain visibility or seed funding can also help burgeoning communities avoid reinventing the wheel.

Furthermore, mentorship from people who have built research communities from the ground up in adjacent fields can be valuable for advising groups on how to grow and address challenges. Knowledgeable mentors can also help groups understand how to sustain a community, an aspect that is often critical to long-term viability.

The GLP was initiated as researchers working on different issues related to land began to connect, forging collaborations that eventually grew into a global network, which itself now comprises a variety of smaller networks, including working groups and regional (nodal) offices. The recently created Early Career Network, launched through webinars and other online communications, is providing a space where young scholars are encouraged to create their own governance structures and articulate what they need in terms of capacity building from the larger community.

Members of the GLP’s Scientific Steering Committee visit an agave farm in Oaxaca in 2024. Credit: Rieley Auger

Growing the GLP has not always been an easy process, however. Sustaining the community has required continually maintaining support and funding from multiple institutions. To date, much of the growth has relied on volunteer work, with members of the GLP’s Scientific Steering Committee, working groups, and nodal offices providing unpaid service above and beyond their existing professional responsibilities. This arrangement of distributed labor underscores the importance of effective coordination for maintaining connections and momentum across the network.

The experiences of the GLP and other groups show that new interdisciplinary communities can start small and run largely on volunteer energy, which we recognize is not something all researchers—especially those early in their career—have to spare. If the communities can then reach a critical mass of participants, they may be able to secure institutional support and professional coordination to help them thrive over the long term.

Harnessing Interdisciplinarity

We came to realize that with our expertise, we can generate innovative ideas that advance science at the intersections between disciplines.

Earlier in our careers, we used to internalize criticisms about not belonging or excelling in any one discipline. Then we came to realize that with our expertise, we can generate innovative ideas that advance science at the intersections between disciplines. Indeed, people with interdisciplinary profiles can fill critical research gaps—and should be seen as assets, not liabilities. Many universities and funders understand this truth at the leadership level, but challenges remain in how interdisciplinarity is evaluated within departments and by hiring, promotion, and grant review panels.

To help move the needle, we actively characterize ourselves as interdisciplinary land system scientists in our tenure and promotion documents, preferring to own the position and emphasize its strengths, rather than to shy away from it. Individuals acting on their own, however, may have only limited influence. That is why building and sustaining communities is so important: They create the collective weight needed to demonstrate value, shift norms, and motivate institutional change.

Within community-building efforts, it is key to create space for participation from researchers with varied backgrounds and experiences. The GLP supports this approach through its distributed subnetworks, including working groups and regional nodes, and by convening international Open Science Meetings on different continents that bring together hundreds of scientists every few years. GLP members frequently present on the program’s work as well as strategies and approaches at other conferences, helping spread the word about the value of growing interdisciplinary communities.

As more researchers connect across disciplinary and geographic boundaries, the scientific enterprise will be better positioned to pursue sustainable solutions that address complex, urgent problems to secure livelihoods and food security for the global population and to safeguard our planet’s biodiversity and environmental health.

References

Andrews, E. J., et al. (2020), Supporting early career researchers: Insights from interdisciplinary marine scientists, ICES J. Mar. Sci., 77(2), 476–485, https://doi.org/10.1093/icesjms/fsz247.

Bentley, A., and R. Garrett (2023), Don’t get mad, get equal: Putting an end to misogyny in science, Nature, 619, 209–211, https://doi.org/10.1038/d41586-023-02101-x.

Berkes, E., et al. (2024), Slow convergence: Career impediments to interdisciplinary biomedical research, Proc. Natl. Acad. Sci. U. S. A., 121(32), e2402646121, https://doi.org/10.1073/pnas.2402646121.

Carrigan, C., and C. D. Wylie (2023), Introduction: Caring for equitable relations in interdisciplinary collaborations, Catalyst Feminism Theory Technosci., 9(2), 1–16, https://doi.org/10.28968/cftt.v9i2.41070.

de Bremond, A., et al. (2019), What role for global change research networks in enabling transformative science for global sustainability? A Global Land Programme perspective, Curr. Opinion Environ. Sustainability, 38, 95–102, https://doi.org/10.1016/j.cosust.2019.05.006.

Haider, L. J., et al. (2018), The undisciplinary journey: Early-career perspectives in sustainability science, Sustainability Sci., 13, 191–204, https://doi.org/10.1007/s11625-017-0445-1.

Liu, M., et al. (2023), Female early-career scientists have conducted less interdisciplinary research in the past six decades: Evidence from doctoral theses, Humanit. Soc. Sci. Commun., 10(1), 918, https://doi.org/10.1057/s41599-023-02392-5.

Marx, V. (2022), Cross-disciplinary ways to connect and blend, Nat. Methods, 19(10), 1149, https://doi.org/10.1038/s41592-022-01622-z.

Watkins, C., et al. (2018), Developing an interdisciplinary and cross‐sectoral community of practice in the domain of forests and livelihoods, Conserv. Biol., 32(1), 60–71, https://doi.org/10.1111/cobi.12982.

Woolston, C. (2021), Discrimination still plagues science, Nature, 600(7887), 177–179, https://doi.org/10.1038/d41586-021-03043-y.

Author Information

Laura Vang Rasmussen (lr@ign.ku.dk), Department of Geosciences and Natural Resource Management, University of Copenhagen, Copenhagen, Denmark; Rachael Garrett, Department of Geography and Conservation Research Institute, University of Cambridge, Cambridge, U.K.; A. Sofia Nanni, Instituto de Ecología Regional, Horco Molle, Yerba Buena, Argentina; also at Facultad de Ciencias Naturales e Instituto Miguel Lillo, Universidad Nacional de Tucumán, San Miguel de Tucumán, Argentina; Navin Ramankutty, School of Public Policy and Global Affairs and Institute for Resources, Environment and Sustainability, University of British Columbia, Vancouver, Canada; and Ariane de Bremond, Global Land Programme, Department of Geographical Sciences, University of Maryland, College Park

Citation: Rasmussen, L. V., R. Garrett, A. S. Nanni, N. Ramankutty, and A. de Bremond (2026), Creating communities to help interdisciplinary scientists thrive, Eos, 107, https://doi.org/10.1029/2026EO260058. Published on 13 February 2026. This article does not represent the opinion of AGU, Eos, or any of its affiliates. It is solely the opinion of the author(s). Text © 2026. The authors. CC BY-NC-ND 3.0
Except where otherwise noted, images are subject to copyright. Any reuse without express permission from the copyright owner is prohibited.

A New Way to Measure Quartz Strength at High Pressure

Fri, 02/13/2026 - 14:00
Editors’ Highlights are summaries of recent papers by AGU’s journal editors. Source: Journal of Geophysical Research: Solid Earth

Quartz is widely thought to control the mechanical strength of Earth’s continental crust, but measuring its strength at high pressure and temperature has long been challenging.

Medina et al. [2026] deform polycrystalline α-quartz at crustal pressure and temperature conditions while directly monitoring stress inside the sample using in situ synchrotron X-ray diffraction. Unlike traditional experiments that rely on external load measurements, this approach derives stress from lattice strain within the quartz itself, avoiding long-standing uncertainties related to friction corrections. The results show that quartz strength varies systematically with temperature, transitioning from lattice-resistance–controlled plasticity below 800 °C to dislocation creep at higher temperatures.

Remarkably, the new measurements are broadly consistent with classic deformation experiments despite the very different experimental techniques. The data also show little pressure dependence over the tested conditions, suggesting that temperature plays the dominant role in controlling quartz strength in much of the crust. These findings provide a more reliable experimental foundation for flow laws used to model crustal deformation, earthquakes, and mountain-building processes.

Citation: Medina, D. A. J., Kaboli, S., Patterson, B. M., & Burnley, P. C. (2026). Strength α-quartz: New results from high pressure in situ X-ray diffraction experiments. Journal of Geophysical Research: Solid Earth, 131, e2025JB032753. https://doi.org/10.1029/2025JB032753

—Jun Tsuchiya, Editor, JGR: Solid Earth

Text © 2026. The authors. CC BY-NC-ND 3.0
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The exceptional occurrence of landslides in the 2025 South Asia summer monsoon

Fri, 02/13/2026 - 07:12

In NW India, rainfall in the 2025 monsoon was 27% above the long term average. Over 2,500 people were killed in India and Pakistan by landslides and floods as a result.

In India and Pakistan, the 2025 summer monsoon generated unusual amount of landslide activity. I described some of these events along the way, most notably in India. In Pakistan, it is much harder to get a good picture of the events that occur in the higher mountain areas.

A new open access paper (Sana et al. 2026) in the journal Landslides provides an initial commentary on these events. By their calculation, 1,528 people were killed in floods and landslides in India and 1,006 were killed in Pakistan.

The paper provides a description of some of the more serious events, which is in itself very helpful, but the most interesting aspect is the consideration of the underlying causes. Across all of India, the total monsoon rainfall was 10% above the long term average, but in Northwest India, which was most seriously impacted area, rainfall was 27% above the long term average. In addition, there was an unusually large number of shorter duration extreme rainfall events, which were primarily responsible for the landslides and floods. This graph, from Sana et al. (2026), provides the 2026 monsoon rainfall record for Mandi district in Himachal Pradesh, for example:-

Rainfall data for the monsoon months of June to August 2025 for Mandi district highlighting cloudburst events. Graph from Sana et al. (2026).

An example of these shorter rainfall events occurred in Khyber Pakhtunkhwa (KP) province between 14 and 25 August 2025, when a succession of cloudbursts triggered landslides and floods in Buner, Swat, Shangla, Mansehra and Dir districts, killing 504 people and leaving thousands more homeless.

But Sana et al. (2026) also remind us that rainfall alone is not the cause of these landslides and floods. Vulnerability has also increased dramatically – for example, there has been a sharp decline in forest cover across much of the area. There has also been growth in urban areas, often with poor planning control, meaning that much of the population is occupying more hazardous locations. And, as I have noted before, poor quality infrastructure development (especially road building) is driving instability across large swathes of hillslopes, rendering them vulnerable to the changed rainfall patterns.

I write on the morning after the decision by the frankly nonsensical decision by the Trump government to reverse the 2009 endangerment finding regarding greenhouse gases, an event that will be judged harshly by future generations. However, in the medium term, this will further exacerbate the issues of increasing rainfall intensities, which drive these horrific events.

It is really helpful that Sana et al. (2026) have provided this intial commentary and analysis of the 2025 monsoon landslides and floods. I will look forward to seeing more detailed analyses in due course.

Reference

Sana, E., Kritika & Kumar, A. 2026. Preliminary investigation of rainfall-induced landslides and related damages by the 2025 extreme monsoon in the Northwestern Himalayan regionLandslides. https://doi.org/10.1007/s10346-026-02703-2

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