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The Water Came From Nowhere': Settlements, Hotels and Farms Flooded in Kenya’s Rift Valley

Dickson Ngome's farm at Lake Naivasha in Kenya's Rift Valley has been submerged due to rising water levels

NAIVASHA, Kenya (AP) — When Dickson Ngome first leased his farm at Lake Naivasha in Kenya’s Rift Valley in 2008, it was over 2 kilometers (1.2 miles) from shore. The farm was on 1.5 acres (0.6 hectares) of fertile land where he grew vegetables to sell at local markets.At the time, the lake was receding and people were worried that it might dry up altogether. But since 2011, the shore has crept ever closer. The rains started early this year, in September, and didn't let up for months.One morning in late October, Ngome and his family woke up to find their home and farm inside the lake. The lake levels had risen overnight and about a foot of water covered everything.“It seemed as if the lake was far from our homes,” Ngome’s wife, Rose Wafula, told The Associated Press. “And then one night we were shocked to find our houses flooded. The water came from nowhere.” Climate change caused increased rains, scientists say The couple and their four children have had to leave home and are camping out on the first floor of an abandoned school nearby.Some 5,000 people were displaced by the rise in Lake Naivasha’s levels this year. Some scientists attribute the higher levels to increased rains caused by climate change, although there may be other factors causing the lake’s steady rise over the past decade.The lake is a tourism hot spot and surrounded by farms, mostly growing flowers, which have gradually been disappearing into the water as the lake levels rise.Rising levels have not been isolated to Naivasha: Kenya’s Lake Baringo, Lake Nakuru and Lake Turkana — all in the Rift Valley — have been steadily rising for 15 years. “The lakes have risen almost beyond the highest level they have ever reached,” said Simon Onywere, who teaches environmental planning at Kenyatta University in Kenya’s capital Nairobi. Rising lake levels displaced tens of thousands A study in the Journal of Hydrology last year found that lake areas in East Africa increased by 71,822 square kilometers (27,730 square miles) between 2011 and 2023. That affects a lot of people: By 2021, more than 75,000 households had been displaced across the Rift Valley, according to a study commissioned that year by the Kenyan Environment Ministry and the United Nations Development Program.In Baringo, the submerged buildings that made headlines in 2020 and 2021 are still underwater.“In Lake Baringo, the water rose almost 14 meters,” Onywere said. “Everything went under, completely under. Buildings will never be seen again, like the Block Hotels of Lake Baringo.” Flower farms taking a beating Lake Naivasha has risen steadily too, “engulfing three quarters of some flower farms,” Onywere said.Horticulture is a major economic sector in Kenya, generating just over a billion U.S. dollars in revenue in 2024 and providing 40% of the volume of roses sold in the European Union, according to Kenya’s Ministry of Foreign Affairs.Significant research has gone into the reasons behind the rising lakes phenomenon: A 2021 study on the rise of Kenya’s Rift Valley lakes was coauthored by Kenyan meteorologist Richard Muita, who is now acting assistant director of the Kenya Meteorological Department.“There are researchers who come up with drivers that are geological, others with reasons like planetary factors,” Muita said. “The Kenya Meteorological Department found that the water level rises are associated with rainfall patterns and temperature changes. When the rains are plentiful, it aligns with the increase in the levels of the Rift Valley lake waters.”Sedimentation is also a factor. “From the research I have read, there’s a lot of sediment, especially from agricultural related activities, that flows into these lakes,” says Muita. ‘A mess’ made by the government years ago Naivasha’s official high water mark was demarcated at 1,892.8 meters (6,210 feet) above sea level by the Riparian Association in 1906, and is still used by surveyors today. That means this year’s flooding was still almost a meter (3 feet) below the high mark.It also means that the community of Kihoto on Lake Naivasha where the Ngomes lived lies on riparian land — land that falls below the high water mark, and can only be owned by the government.“It’s a mess established by the government … towards the late 1960s,” said Silas Wanjala, general manager of the Lake Naivasha Riparian Association, which was founded some 120 years ago and has been keeping meticulous records of the lake’s water levels since.Back then, a farmer was given a “temporary agricultural lease” on Kihoto, said Wanjala. When it later flooded and the farmer packed up and left, the farmworkers stayed on the land and later applied for subdivisions, which were approved. In the 60-odd years since, a whole settlement has grown on land that is officially not for lease or sale. This also isn’t the first time it’s been flooded, said Wanjala. It's just very rare that the water comes up this high. That’s little consolation for the people who have been displaced by this year’s floods and now cannot go home without risking confrontations with hippopotamuses.To support those people, the county is focusing its efforts on where the need is greatest.“We are tackling this as an emergency," says Joyce Ncece, chief officer for disaster management in Nakuru County, which oversees Lake Naivasha. “The county government has provided trucks to help families relocate. We have been helping to pay rent for those who lack the finances.”Scientists like Onywere and Muita are hoping for longer-term solutions. “Could we have predicted this so that we could have done better infrastructure in less risk-prone areas?” Onywere said.Muita wants to see a more concerted global effort to combat climate change, as well as local, nature-based solutions centered on Indigenous knowledge, such as “conservation agriculture, where there is very limited disturbance of the land,” to reduce sedimentation of the lakes.But all of this is of little help to Ngome and Wafula, who are still living at the school with their children. As the rest of the world looks forward to the holidays and new year, their future is uncertain. Lake Naivasha’s continuous rise over the past 15 years does not bode well: They have no idea when, or if, their farm will ever be back on dry land. The Associated Press receives financial support for global health and development coverage in Africa from the Gates Foundation. The AP is solely responsible for all content. Find AP’s standards for working with philanthropies, a list of supporters and funded coverage areas at AP.org.Copyright 2025 The Associated Press. All rights reserved. This material may not be published, broadcast, rewritten or redistributed.Photos You Should See – December 2025

Disaster after disaster: do we have enough raw materials to ‘build back better’?

Disasters like earthquakes and flood destroy homes and generate vast amounts of waste. Is there a better, greener way to rebuild affected communities?

This Christmas Day marks 21 years since the terrifying Indian Ocean tsunami. As we remember the hundreds of thousands of lives lost in this tragic event, it is also a moment to reflect on what followed. How do communities rebuild after major events such as the tsunami, and other disasters like it? What were the financial and hidden costs of reconstruction? Beyond the immediate human toll, disasters destroy hundreds of thousands of buildings each year. In 2013, Typhoon Haiyan damaged a record 1.2 million structures in Philippines. Last year, earthquakes and cyclones damaged more than half a million buildings worldwide. For communities to rebuild their lives, these structures must be rebuilt. While governments, non-government agencies and individuals struggle to finance post-disaster reconstruction, rebuilding also demands staggering volumes of building materials. In turn, these require vast amounts of natural resource extraction. For instance, an estimated one billion burnt clay bricks were needed to reconstruct the half-million homes destroyed in the Nepal earthquake. This is enough bricks to circle the Earth six times if laid end to end. How can we responsibly source such vast quantities of materials to meet demand? Demand causes problems Sudden spikes in demand have led to severe shortages of common building materials after nearly every major disaster over the past two decades, including the 2015 Nepal earthquake and the 2019 California wildfires. These shortages often trigger price hikes of 30–40%, which delays reconstruction and prolongs the suffering of affected communities. Disasters not only increase demand for building materials but also generate enormous volumes of debris. For example, the 2023 Turkey–Syria earthquake produced more than 100 million cubic meters of debris – 40 times the volume of the Great Pyramid of Giza. Disaster debris can pose serious environmental and health risks, including toxic dust and waterway pollution. But some debris can be safely transformed into useful assets such as recycled building materials. Rubble can be crushed and repurposed as base for low-traffic roads or turned into cement blocks . The consequences of poor post-disaster building materials management have reached alarming global proportions. After the 2004 Indian Ocean Tsunami, for example, the surge in sand demand led to excessive and illegal sand mining in rivers along Sri Lanka’s west coast. This caused irreversible ecological damage to two major watersheds, devastating the livelihoods of thousands of farmers and fisherpeople. Similar impacts from the overextraction of materials such as sand, gravel, clay and timber have been reported following other major disasters, including the 2008 Sichuan earthquake in China and Cyclone Idai in Mozambique in 2019. If left unaddressed, the social, environmental and economic impacts of resource extraction will escalate to catastrophic levels, especially as climate change intensifies disaster frequency. Urgent need for action This crisis has yet to receive adequate international attention. Earlier this year, several global organisations came together to publish a Global Call to Action on sustainable building materials management after disasters. Based on an analysis of 15 major disasters between 2005 and 2020, it identified three key challenges: building material shortages and price escalation, unsustainable extraction and use of building materials, and poor management of disaster debris. Although well-established solutions exist to address these challenges, rebuilding efforts suffer from policy and governance gaps. The Call to Action urges international bodies such as the United Nations Office for Disaster Risk Reduction to take immediate policy and practical action. Building back better and safer After a disaster hits, it leaves an opportunity to build back better. Rebuilding can boost resilience to future hazards, encourage economic development and reduce environmental impact. The United Nations’ framework for disaster management emphasises the importance of rebuilding better and safer rather than simply restoring communities to pre-disaster conditions. Disaster affected communities should be rebuilt with capacity to cope with future external shocks and environmental risks. Lessons can be learned from both negative and positive experiences of past disasters. For example, poor planning of some reconstruction projects after the Indian ocean Tsunami (2004) in Sri Lanka made the communities vulnerable again to coastal hazards within a few years. On the other hand, the community-led reconstruction approach followed after the Bhuj earthquake, India (2001), has resulted in safer and more socio-economically robust settlements, standing the test of 24 years. As an integral part of the “build back better” approach, authorities must include strategies for environmentally and socially responsible management of building materials. These should encourage engineers, architects and project managers to select safe sustainable materials for reconstruction projects. At the national level, regulatory barriers to repurposing disaster debris should be removed, whilst still ensuring safe management of hazardous materials such as asbestos. For example, concrete from fallen buildings was successfully used as road-base and as recycled aggregate for infrastructure projects following the 2004 tsunami in Indonesia and 2011 Tohoku Earthquake in Japan. This critical issue demands urgent public and political attention. Resilient buildings made with safe sustainable material will save lives in future disasters. Missaka Nandalochana Hettiarachchi receives funding from WWF, an environmental NGO, through his role in disaster management

A damaged King County levee awaited fixes for years. Then it failed

As an atmospheric river slammed into the Pacific Northwest, water burst through a damaged levee in Washington.

As rainfall inundated the Pacific Northwest this month, swelling the region’s rivers to record levels, the Desimone levee seemed destined to fail.Severe flooding in 2020 had damaged the 2.2-mile earthen barrier near Tukwila. Muddy waters from the Green River bubbled up on the opposite side and seeped into nearby properties. A King County report months later described the levee’s weakened state as the “most important issue” on the river’s lower reach.The years that followed were filled with red tape and bureaucratic infighting among the agencies most responsible for the region’s levee system: King County, its flood control district and the U.S. Army Corps of Engineers. All the while, cities in the flood plain clamored for help, and the Desimone awaited repair.Construction was set to begin this summer, but the Corps pulled out of the work in January, revoking promised federal funding and setting the project back years, according to interviews and public records obtained by The Seattle Times.Reagan Dunn, chair of the district’s advisory committee and a Metropolitan King County Council member, described a pattern of “tension” between the flood control district and the Corps.This month’s back-to-back atmospheric rivers pushed the levee system like never before. The Desimone was the first of two to fail.Earlier in the series of storms, water had once again begun to seep through Desimone’s earthen barrier, which shields a mostly commercial and industrial hub in Tukwila. On Monday, the river tore its way through, sparking a widespread evacuation. Officials feared the ensuing flash flood might be deadly. Workers plugged the hole quickly. Knowing the levee’s risk, they had already been watching the site for days. No injuries were reported in the breach.The patchwork nature of repairs at Desimone, and levees like it, illuminates the growing challenge of protecting Western Washington communities from flooding worsened by climate change.For generations, Washington has relied on levees as a simple solution to a complex problem, said Alan Hamlet, a former Seattle resident and scientist who now works as an associate professor of civil and environmental engineering at the University of Notre Dame. Explosive growth behind them has combined with an overarching desire to spend the minimum required for flood protection, he said. That often means deferring costlier long-term maintenance, mitigation and upgrades of these emergency barriers in favor of more pressing needs. This has resulted in higher risks for the very communities the levees were designed to protect.The state, and much of the country, stands at the nexus of that growth behind the walls of inadequate infrastructure to keep natural disasters at bay, Hamlet said.“Put all those things together and you have a hidden crisis that is going to begin to express itself more and more frequently,” Hamlet said.The 18-year-old King County Flood Control District shuffles its priority levees based on disrepair that changes with the weather. The district has started to plan for the long term, but in its earliest years, it focused on inexpensive and easy fixes in high-risk areas, Dunn said.“In other words, low-hanging fruit,” he said.Flooding in Washington state 2025Bureaucratic tangleThe Desimone levee has been damaged and repaired multiple times over the past six decades. Most recently, years of disagreements among agencies dragged out Desimone’s renovation.The flood control district asked the Corps to step in not long after the 2020 flood. High waters in the Green River then had not only left water seeping through the levee in at least three places, but also bubbling up from underneath.Federal officials agreed to spearhead a plan to repair the levee and cover 80% of the cost. It proposed estimates up to $16.6 million for a project focused solely on restoring the levee to its preflood condition, records show.Such is frequently the case for levee systems nationwide, Hamlet said. Restoring them to their original condition is typically less expensive and complicated. Expanding them or exploring other options takes more time, money and political will.But the flood district wanted more for Desimone: a design that would fix the damage and relieve water pressure further by setting the levee back, restoring some of the river’s natural bank. It was projected to cost the district about $30 million.The district’s plan would take longer and cost more but reduce long-term risks, said Michelle Clark, the district’s director. “We want to do a bigger project so that we’re not coming back to do more repairs.”The flood control district handles planning, but the project hinged on King County finding land along the river for the new work, records show. But it fell short.These types of repairs are more complicated than they might seem, Hamlet said. Strengthen a levee in one place, and you’ll send floodwaters careening into another. Set a levee back from the river, or remove one to restore a flood plain, and first you have to clear out any homes or businesses already there. These structures aren’t the only way to hold back floodwaters, but in many places, they’re the system that’s already there.A failed dealThe Corps worked in fits and starts, at one point in 2022 halting its involvement due to staffing challenges. Even when the county made headway securing land, the Corps said it had used the wrong language in the agreements. At the same time, the county accused the Corps of clerical errors that dragged out the planning process, according to county records.The county — officials for which said they were unable to immediately comment, citing the ongoing flood emergency — was confident it could secure the land, just not on schedule, according to a county brief from April. It proposed breaking ground in 2026 instead.Citing the county’s “inability” to provide the needed land along the highly developed and industrial area, the Corps backed out of the agreement in a January letter.“We have been pushing them since 2020,” Clark said. “And it’s frustrating.”The Corps “worked diligently with King County” but couldn’t move forward without land for construction, the agency wrote in an email to The Times. Levee rehabilitation can be “complex,” it added. “The federal process, sponsor timelines and real estate actions do not always align well, but we are committed to finding a solution when possible,” the agency wrote.Abandoned by the Corps, the county and its partner cities faced their biggest setback, Clark said.Everybody blamed each other as the flood season approached.Concerns heightened after the Corps pulled its support. In July, city leaders from Tukwila, Kent and Renton asked the flood district to more immediately prioritize the levee repair project.Tukwila officials declined to comment, and Kent and Renton officials did not respond to a request for comment by publication time.As the fall rains approached — and without significant improvements on the levee — officials from Tukwila, Kent, King County and the Corps of Engineers spoke in late October to review the contingency plan in case the structure failed, according to Tukwila city records. They walked the levee bank to flag logistical challenges and clarified roles and responsibilities in case of an emergency.The Corps passed along its nearly complete project design for the Desimone levee, according to its January letter to the district. But without the federal government to offset the cost, the county’s grand plan was too pricey. The district has years of research and $25 million set aside for the levee repairs, but it might not be enough, Clark said; it needs to prepare options before it can move forward with a plan.The King County Flood Control District is now, in many ways, exactly where it was in 2020: waiting for the water to recede, preparing to assess the damage and on the verge of once again planning how to fix the Desimone.--Conrad Swanson and Lulu Ramadan© 2025 The Seattle Times. Visit www.seattletimes.com. Distributed by Tribune Content Agency, LLC.

You think you’ve seen a big tree? Why we can no longer recognize a real forest

Environmental educator Ross Reid, also known as Nerdy About Nature, explains why we don't understand the scale of true old-growth forests.

Stand in awe before a towering Douglas fir in an Oregon forest, and you might believe you’re experiencing the majesty of old growth. But according to environmental educator Ross Reid, what most of us consider impressive forest landscapes are merely shadows of what once existed. In an archived episode of the Peak Northwest podcast, Reid, who is known for his presence on social media as “Nerdy About Nature,” explains why our perception of forests has been fundamentally altered by what we’ve lost.“It’s this concept known as shifting baseline syndrome where we’re limited in what we think is normal based on our experiences,” Reid said on the podcast. “The people who are living in this part of the world a hundred years ago had a radically different perception of the forest around them versus the one we have now.”Generative AI was used to summarize a recent episode of the Peak Northwest podcast. This story was reviewed and edited by The Oregonian/OregonLive.This psychological phenomenon, where each generation accepts a more diminished version of nature as “normal,” has profound implications for conservation efforts, Reid said. If we can’t recognize what we’ve lost, how can we work to protect or restore it?Bushwhacking through the rain forest of the Devil's Staircase Wilderness, one of Oregon's last true old-growth forests, in the Coast Range.Jamie Hale/The OregonianReid offered tangible examples of the differences between second-growth and old-growth forests that go beyond just tree size. “Pit mound topography is a concept in an old growth forest where you have bigger, older trees falling over naturally ... and you end up with a really undulating bit of terrain,” Reid said. “A lot of the forests we have in the Pacific Northwest, especially the second growth ones, you walk around, it’s fairly easy to walk off trail because it’s all kind of flat.”Throughout the episode, Reid explained how old-growth forests create unique habitats that are impossible to replicate in younger stands. For instance, bears in British Columbia rely on hollowed-out cavities in old Western red cedar trees for denning — structures that take centuries to form.A towering western redcedar tree is the highlight of the Rockaway Beach Old Growth Cedar Preserve on the north Oregon coast.Jamie Hale/The OregonianThe conversation reveals how industrial forestry has not just changed how forests look, but fundamentally altered their ecological function. Second-growth forests managed for timber production lack the structural complexity, genetic diversity, and ecological relationships that develop in forests allowed to mature naturally over centuries, Reid said.For anyone who loves hiking through Pacific Northwest forests, the interview offers a new lens through which to view familiar landscapes. Reid challenges listeners to look beyond their initial impressions of big trees and green canopies to recognize the subtler signs of ecological complexity that distinguish truly ancient forests from their younger counterparts.Listen to the full episode here: Subscribe to The Oregonian/OregonLive’s travel and outdoors podcast Peak Northwest on Apple, Spotify, YouTube or anywhere else you listen to podcasts. Hosts Jamie Hale and Chiara Profenna take you to some of the greatest destinations in Oregon and the Pacific Northwest. Check out more Peak Northwest episodes below.

This Climate Concern Is Way Out There

This story was originally published by Yale e360 and is reproduced here as part of the Climate Desk collaboration. On a mid-November evening, at precisely 7:12 p.m., a SpaceX Falcon 9 rocket lifted off from Cape Canaveral Space Force Station on the Florida coast. It appeared to be a perfect launch. At an altitude of about 40 […]

This story was originally published by Yale e360 and is reproduced here as part of the Climate Desk collaboration. On a mid-November evening, at precisely 7:12 p.m., a SpaceX Falcon 9 rocket lifted off from Cape Canaveral Space Force Station on the Florida coast. It appeared to be a perfect launch. At an altitude of about 40 miles, the rocket’s first stage separated and fell back to Earth, eventually alighting in a gentle, controlled landing on a SpaceX ship idling in the Atlantic Ocean. The mission’s focus then returned to the rocket’s payload: 29 Starlink communication satellites that were to be deployed in low-Earth orbit, about 340 miles above the planet’s surface. With this new fleet of machines, Starlink was expanding its existing mega-constellation so that it numbered over 9,000 satellites, all circling Earth at about 17,000 miles per hour.  Launches like this have become commonplace. As of late November, SpaceX had sent up 152 Falcon 9 missions in 2025—an annual record for the company. And while SpaceX is the undisputed leader in rocket launches, the space economy now ranges beyond American endeavors to involve orbital missions—military, scientific, and corporate—originating from Europe, China, Russia, India, Israel, Japan, and South Korea. This year the global total of orbital launches will near 300 for the first time, and there seems little doubt it will continue to climb.     “We are now in this regime where we are doing something new to the atmosphere that hasn’t been done before.” Starlink has sought permission from the Federal Communications Commission to expand its swarm, which at this point comprises the vast majority of Earth’s active satellites, so that it might within a few years have as many as 42,000 units in orbit. Blue Origin, the rocket company led by Jeff Bezos, is in the early stages of helping to deploy a satellite network for Amazon, a constellation of about 3,000 units known as Amazon Leo. European companies, such as France’s Eutelsat, plan to expand space-based networks, too. “We’re now at 12,000 active satellites, and it was 1,200 a decade ago, so it’s just incredible,” Jonathan MacDowell, a scientist at Harvard and the Smithsonian who has been tracking space launches for several decades, told me recently. MacDowell notes that based on applications to communications agencies, as well as on corporate projections, the satellite business will continue to grow at an extraordinary rate. By 2040, it’s conceivable that more than 100,000 active satellites would be circling Earth. But counting the number of launches and satellites has so far proven easier than measuring their impacts. For the past decade, astronomers have been calling attention to whether so much activity high above might compromise their opportunities to study distant objects in the night sky. At the same time, other scientists have concentrated on the physical dangers. Several studies project a growing likelihood of collisions and space debris—debris that could rain down on Earth or, in rare cases, on cruising airplanes. More recently, however, scientists have become alarmed by two other potential problems: the emissions from rocket fuels, and the emissions from satellites and rocket stages that mostly ablate (that is, burn up) on reentry. “Both of these processes are producing pollutants that are being injected into just about every layer of the atmosphere,” explains Eloise Marais, an atmospheric scientist at University College London, who compiles emissions data on launches and reentries.  As Marais told me, it’s crucial to understand that Starlink’s satellites, as well as those of other commercial ventures, don’t stay up indefinitely. With a lifetime usefulness of about five years, they are regularly deorbited and replaced by others. The new satellite business thus has a cyclical quality: launch, deploy, deorbit, destroy. And then repeat.  The cycle suggests we are using Earth’s mesosphere and stratosphere—the layers above the surface-hugging troposphere—as an incinerator dump for space machinery. Or as Jonathan MacDowell puts it: “We are now in this regime where we are doing something new to the atmosphere that hasn’t been done before.” MacDowell and some of his colleagues seem to agree that we don’t yet understand how—or how much—the reentries and launches will alter the air. As a result, we’re unsure what the impacts may be to Earth’s weather, climate, and (ultimately) its inhabitants.  To consider low-Earth orbit within an emerging environmental framework, it helps to see it as an interrelated system of cause and effect. As with any system, trying to address one problematic issue might lead to another. A long-held idea, for instance, has been to “design for demise,” in the argot of aerospace engineers, which means constructing a satellite with the intention it should not survive the heat of reentry. “But there’s an unforeseen consequence of your solution unless you have a grasp of how things are connected,” according to Hugh Lewis, a professor of astronautics at the University of Birmingham in the United Kingdom. In reducing “the population of debris” with incineration, Lewis told me—and thus, with rare exceptions, saving us from encounters with falling chunks of satellites or rocket stages—we seem to have chosen “probably the most harmful solution you could get from a perspective of the atmosphere.”  We don’t understand the material composition of everything that’s burning up. Yet scientists have traced a variety of elements that are vaporizing in the mesosphere during the deorbits of satellites and derelict rocket stages; and they’ve concluded these vaporized materials—as a recent study in the Proceedings of the National Academy of Sciences put it—“condense into aerosol particles that descend into the stratosphere.” The PNAS study, done by high altitude air sampling and not by modeling, showed that these tiny particles contained aluminum, silicon, copper, lead, lithium, and more exotic elements like niobium. “Emission plumes from the first few minutes of a mission, which disperse into the stratosphere, may…have a significant effect on the ozone layer.” The large presence of aluminum, signaling the formulation of aluminum oxide nanoparticles, may be especially worrisome, since it can harm Earth’s protective ozone layers and may undo our progress in halting damage done by chlorofluorocarbons, or CFCs. A recent academic study in the journal Geophysical Research Letters concluded that the ablation of a single 550-pound satellite (a new Starlink unit is larger, at about 1,800 pounds) can generate around 70 pounds of aluminum oxide nanoparticles. This floating metallic pollution may stay aloft for decades.  The PNAS study and others, moreover, suggest the human footprint on the upper atmosphere will expand, especially as the total mass of machinery being incinerated ratchets up. Several scientists I spoke with noted that they have revised their previous belief that the effects of ablating satellites would not exceed those of meteorites that naturally burn up in the atmosphere and leave metallic traces in the stratosphere. “You might have more mass from the meteoroids,” Aaron Boley, an astronomer at the University of British Columbia, said, but “these satellites can still have a huge effect because they’re so vastly different [in composition].”  Last year, a group of researchers affiliated with NASA formulated a course of research that could be followed to fill large “knowledge gaps” relating to these atmospheric effects. The team proposed a program of modeling that would be complemented by data gleaned from in situ measurements. While some of this information could be gathered through high-altitude airplane flights, sampling the highest-ranging air might require “sounding” rockets doing tests with suborbital flights. Such work is viewed as challenging and not inexpensive—but also necessary. “Unless you have the data from the field, you cannot trust your simulations too much,” Columbia University’s Kostas Tsigaridis, one of the scientists on the NASA team, told me.  Tsigaridis explains that lingering uncertainty about NASA’s future expenditures on science has slowed US momentum for such research. One bright spot, however, has been overseas, where ESA, the European Space Agency, held an international workshop in September to address some of the knowledge gaps, particularly those relating to satellite ablations. The ESA meeting resulted in a commitment to begin field measurement campaigns over the next 24 months, Adam Mitchell, an engineer with the agency, said. The effort suggests a sense of urgency, in Europe, at least, that the space industry’s growth is outpacing our ability to grasp its implications. A SpaceX Falcon 9 rocket takes off. SpaceX now has more than 9,000 Starlink satellites orbiting the Earth.SpaceX The atmospheric pollution problem is not only about what’s raining down from above, however; it also relates to what happens as rockets go up. According to the calculations of Marais’ UCL team, the quantity of heat-trapping gases like CO2 produced during liftoffs are still tiny in comparison to, say, those of commercial airliners. On the other hand, it seems increasingly clear that rocket emission plumes from the first few minutes of a mission, which disperse into the stratosphere, may, like reentries, have a significant effect on the ozone layer.  The most common rocket fuel right now is a highly refined kerosene known as RP-1, which is used by vehicles such as SpaceX’s Falcon 9. When RP-1 is burned in conjunction with liquid oxygen, the process releases black carbon particulates into the stratosphere. A recent study led by Christopher Maloney of the University of Colorado used computer models to assess how the black carbon absorbs solar radiation and whether it can warm the upper atmosphere significantly. Based on space industry growth projections a few decades into the future, these researchers concluded that the warming effect of black carbon would raise temperatures in the stratosphere by as much as 1.5 degrees C, leading to significant ozone reductions in the Northern Hemisphere. When satellite companies talk about sustainability, “what they mean is, we want to sustain this rate of growth.”  It may be the case that a different propellant could alleviate potential problems. But a fix isn’t as straightforward as it seems. Solid fuels, for instance, which are often used in rocket boosters to provide additional thrust, emit chlorine—another ozone-destroying element. Meanwhile, the propellant of the future looks to be formulations of liquefied natural gas (LNG), often referred to as liquid methane. Liquid methane will be used to power SpaceX’s massive Starship, a new vehicle that’s intended to be used for satellite deployments, moon missions, and, possibly someday, treks to Mars.  The amount of black carbon emissions from burning LNG may be 75 percent less than from RP-1. “But the issue is that the Starship rocket is so much bigger,” UCL’s Marais says. “There’s so much more mass that’s being launched.” Thus, while liquid methane might burn cleaner, using immense quantities of it—and using it for more frequent launches—could undermine its advantages. Recently, executives at SpaceX’s Texas factory have said they would like to build a new Starship every day, readying the company for a near-constant cycle of launches. One worry amongst scientists is that if new research suggests that space pollution is leading to serious impacts, it may eventually resemble an airborne variation of plastics in the ocean. A more optimistic view is that these are the early days of the space business, and there is still time for solutions. Some of the recent work at ESA, for instance, focuses on changing the “design for demise” paradigm for satellites to what some scientists are calling “design to survive.” Already, several firms are testing satellites that can get through an reentry without burning up; a company called Atmos, for instance, is working on an inflatable “atmospheric decelerator” that serves as a heat shield and parachute to bring cargo to Earth. Satellites might be built from safer materials, such as one tested in 2024 by Japan’s space agency, JAXA, made mostly from wood.  More ambitious plans are being discussed: Former NASA engineer Moriba Jah has outlined a design for an orbital “circular economy” that calls for “the development and operation of reusable and recyclable satellites, spacecraft, and space infrastructure.” In Jah’s vision, machines used in the space economy should be built in a modular way, so that parts can be disassembled, conserved, and reused. Anything of negligible worth would be disposed of responsibly. Most scientists I spoke with believe that a deeper recognition of environmental responsibilities could rattle the developing structure of the space business. “Regulations often translate into additional costs,” says UCL’s Marais, “and that’s an issue, especially when you’re privatizing space.” A shift to building satellites that can survive reentry, for instance, could change the economics of an industry that, as astronomer Aaron Boley notes, has been created to resemble the disposable nature of the consumer electronics business. Boley also warns that technical solutions are likely only one aspect of avoiding dangers and will not address all the complexities of overseeing low-Earth orbit as a shared and delicate system. It seems possible to Boley that in addition to new fuels, satellite designs, and reentry schemes, we may need to look toward quotas that require international management agreements. He acknowledges that this may seem “pie in the sky”; while there are treaties for outer space, as well as United Nations guidelines, they don’t address such governance issues. Moreover, the emphasis in most countries is on accelerating the space economy, not limiting it. And yet, Boley argues that without collective-action policy responses we may end up with orbital shells so crowded that they exceed a safe carrying capacity.  That wouldn’t be good for the environment or society—but it wouldn’t be good for the space business, either. Such concerns may be why those in the industry increasingly discuss a set of principles, supported by NASA, that are often grouped around the idea of “space sustainability.” University of Edinburgh astronomer Andrew Lawrence told me that the phrase can be used in a way that makes it unclear what we’re sustaining: “If you look at the mission statements that companies make, what they mean is, we want to sustain this rate of growth.”  But he doesn’t think we can. As one of the more eloquent academics arguing for space environmentalism, Lawrence perceives an element of unreality in the belief that in accelerating space activity we can “magically not screw everything up.” He thinks a goal in space for zero emissions, or zero impact, would be more sensible. And with recent private-sector startups suggesting that we should use space to build big data centers or increase sunlight on surface areas of Earth, he worries we are not entering an era of sustainability but a period of crisis. Lawrence considers debates around orbital satellites a high-altitude variation on climate change and threats to biodiversity—an instance, again, of trying to seek a balance between capitalism and conservation, between growth and restraint. “Of course, it affects me and other professional astronomers and amateur astronomers particularly badly,” he concedes. “But it’s really that it just wakes you up and you think, ‘Oh, God, it’s another thing. I thought, you know—I thought we were safe.’” After a pause, he adds, “But no, we’re not.”

In Antarctica, Photos Show a Remote Area Teeming With Life Amid Growing Risks From Climate Change

Antarctica, one of the most remote places on Earth, teems with life

ANTARCTICA (AP) — The Southern Ocean is one of the most remote places on Earth, but that doesn't mean it is tranquil. Tumultuous waves that can swallow vessels ensure that the Antarctic Peninsula has a constant drone of ocean. While it can be loud, the view is serene — at first glance, it is only deep blue water and blinding white ice.Several hundred meters (yards) off the coast emerges a small boat with a couple dozen tourists in bright red jackets. They are holding binoculars, hoping for a glimpse of the orcas, seals and penguins that call this tundra home.They are in the Lemaire Channel, nicknamed the “Kodak Gap,” referring to the film and camera company, because of its picture-perfect cliffs and ice formations. This narrow strip of navigable water gives anybody who gets this far south a chance to see what is at stake as climate change, caused mainly by the burning of oil, gas and coal, leads to a steady rise in global average temperatures. The Antarctic Peninsula stands out as one of the fastest warming places in the world. The ocean that surrounds it is also a major repository for carbon dioxide, a greenhouse gas that contributes to warming. It captures and stores roughly 40% of the CO2 emitted by humans, according to the National Oceanic and Atmospheric Administration. On a recent day, Gentoo penguins, who sport slender, orange beaks and white spots above their eyes, appeared to be putting on a show. They took breaks from their dives into the icy water to nest on exposed rock. As the planet warms, they are migrating farther south. They prefer to colonize rock and fish in open water, allowing them to grow in population.The Adelie penguins, however, don't have the same prognosis. The plump figures with short flippers and wide bright eyes are not able to adapt in the same way. By 2100, 60% of Adelie penguin colonies around Antarctica could threatened by warming, according to one study. They rely on ice to rest and escape predators. If the water gets too warm, it will kill off their food sources. From 2002 to 2020, roughly 149 billion metric tons of Antarctic ice melted per year, according to the National Aeronautics and Space Administration. For tourists, Antarctica is still a giant, glacial expanse that is home to only select species that can tolerate such harsh conditions. For example, in the Drake Passage, a dangerous strip of tumultuous ocean, tourists stand in wonder while watching orca whales swim in the narrow strip of water and Pintado petrels soar above. The majestic views in Antarctica, however, will likely be starkly different in the decades ahead. The growing Gentoo penguin colonies, the shrinking pieces of floating ice and the increasing instances of exposed rock in the Antarctic Peninsula all underscore a changing landscape. Associated Press writer Caleigh Wells contributed to this report from Cleveland. The Associated Press’ climate and environmental coverage receives financial support from multiple private foundations. AP is solely responsible for all content. Find AP’s standards for working with philanthropies, a list of supporters and funded coverage areas at AP.org.Copyright 2025 The Associated Press. All rights reserved. This material may not be published, broadcast, rewritten or redistributed.Photos You Should See – December 2025

A California Fisherman May Have Broken Records by Catching a 10.25-Pound Canary Rockfish

A Northern California fisherman may have set state and world records by catching a canary rockfish he says weighed in at 10.25 pounds

SAN FRANCISCO (AP) — A Northern California man caught a plump canary rockfish he says weighed in at 10.25 pounds (4.65 kilograms), likely setting state and world records.Mendocino County fisherman Brendan Walsh, 26, said he caught the fish Tuesday off the coast of Albion, about 150 miles (240 kilometers) north of San Francisco.Walsh was headed back with his father Will Walsh after catching a few yellowtail on a cold and rainy day when he decided to make one last stop at a deeper spot. That's where the younger Walsh landed the canary rockfish.“It was a fluke,” he said. “I’ve never seen anything like it.”Canary rockfish can grow up to 2.5 feet (0.76 meters) in length and weigh 10 lbs. (4.5 kilograms), according to the National Oceanic and Atmospheric Administration. Walsh says the ones he usually catches are small and scrawny, clocking in around 3 lbs. (1.4 kilograms). Walsh said the fish he caught this week was 2.25 feet (0.68 meters) long. He submitted the catch to the California Department of Fish and Wildlife, which tracks angling and diving records. The current state record-holding fish weighed in at 9 lbs. and was caught last November, also in Mendocino County. The department has a form and instructions for submitting a possible record catch, including the names and phone numbers of witnesses. Applicants are asked to contact the department for the nearest environmental scientist who can identify the catch.Walsh said they weighed the fish at an authorized fish market nearby and a state fish and wildlife scientist who works in the area came over to sign off on the paperwork.Walsh has also submitted his catch to the International Game Fish Association in Florida, where the world record holding 10-pound canary rockfish was caught in 1986. He says larger fish may have been caught but never submitted for record consideration. The game fish association did not respond Friday to a request for comment. After spending Tuesday making sure they had taken the right measurements to document the catch, Walsh's mother, Deirdre Lamb, fried the rockfish with garlic and butter to eat on Wednesday.The rockfish was delicious, he said. Copyright 2025 The Associated Press. All rights reserved. This material may not be published, broadcast, rewritten or redistributed.Photos You Should See – December 2025

Dakota Access Pipeline Should Continue Operating, US Army Corps of Engineers Says

By Georgina McCartneyHOUSTON, Dec 19 (Reuters) - The ‌U.S. ​Army Corps of ‌Engineers on Friday released a long-anticipated Environmental Impact ​...

HOUSTON, Dec 19 (Reuters) - The ‌U.S. ​Army Corps of ‌Engineers on Friday released a long-anticipated Environmental Impact ​Statement for the Dakota Access Pipeline (DAPL), recommending that operations of the ‍oil pipeline continue with ​some conditions.The EIS, a document required by U.S. law ​to ⁠evaluate the environmental effects of major federal actions, is a win for DAPL operator Energy Transfer and a step closer to the end of a lengthy court battle between the company and ‌nearby Native American tribes, who have been fighting for ​the pipeline's ‌closure.The document recommends the continued ‍operation ⁠of DAPL, on the grounds that safeguards are put in place such as groundwater monitoring, fish tissue residue analyses and water and sediment sampling, as well as the deployment of new leak detection technology.A U.S. court in 2022 ordered the federal government to undertake a more intensive ​EIS of the 1,100-mile (1,800-km) crude pipeline's route as part of the dispute between Energy Transfer and the tribes who have cited risks to water quality as the pipeline runs through Lake Oahe, with the crossing around half a mile north of the Standing Rock Sioux Reservation.The pipeline has continued to operate while the review is being carried out. It is the biggest oil pipeline ​from the Bakken shale oil basin and can transport up to 750,000 barrels of oil per day from North Dakota to Illinois.It is not known whether USACE's ​recommendation will be implemented. (Reporting by Georgina McCartney in Houston; Editing by Paul Simao)Copyright 2025 Thomson Reuters.

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