Over half of global coastal settlements are retreating inland due to intensifying climate risks

Hurricane Florence moved toward the U.S. East Coast as it intensified to a Category 4 storm, with one-minute sustained winds of 130 mph Monday September 10, 2018. This image, captured by the GOES East satellite at 10:00 am ET, showed Florence in the western Atlantic, about 600 miles southeast of Bermuda, at Category 3 intensity. The storm had developed a small but well-defined eye and a symmetrical appearance typical of major hurricanes that are rapidly intensifying.
Image Credit: NOAA

For centuries, coastlines have attracted dense human settlement and economic activity. Today, more than 40 percent of the global population lives within 100 kilometers of the coast, facing accelerating sea-level rise, coastal erosion, flooding, and tropical cyclones. 

Although moving away from the coast - known as “retreat” - is often viewed as an adaptive strategy, its global extent and drivers have remained unclear. A new study published in Nature Climate Change fills this gap by providing the first global evidence that coastal retreat is driven more by social and infrastructural vulnerability than by historical exposure to hazards. 

The study was conducted by an international team led by researchers from Sichuan University and included remote sensing experts from the University of Copenhagen (Alexander Prishchepov and Shengping Ding, IGN). It maps settlement movements across 1,071 coastal regions in 155 countries. By integrating nighttime light observations with global socioeconomic datasets, the researchers found that 56% of coastal regions have retreated from the coast from 1992 to 2019, and 16% of regions, including the Copenhagen area in Denmark, have moved closer to the coast, while 28% have remained stable. 

The seamounts of Cape Verde: a biodiversity hotspot and a priority for marine conservation in the central-eastern Atlantic

Image Credit: Projecte Luso/iMirabilis2/iAtlantic

An international team led by Covadonga Orejas, a researcher at the Gijón Oceanographic Centre of the Spanish Institute of Oceanography (IEO-CSIC); Veerle Huvenne, a researcher at the UK National Oceanography Centre (NOC); and Jacob González-Solís, professor at the Faculty of Biology and the Biodiversity Research Institute (IRBio) of the University of Barcelona, has published the first comprehensive study on the seamounts of the Cape Verde archipelago, their biodiversity, ecological functionality and socio-economic relevance in the journal Progress in Oceanography.

These volcanic formations — at least 14 large mountains and numerous smaller elevations — act as veritable oases of life in the deep ocean, concentrating nutrients and modifying the circulation of underwater currents. This supports exceptional biodiversity, ranging from microorganisms to communities of deep-sea corals and sponges, as well as sharks, turtles, seabirds and cetaceans. Their position between the temperate waters of the North Atlantic and the tropical waters of the South, further enhances their productivity and ecological connectivity. 

Antarctic mountains could boost ocean carbon absorption

Glaciers transport sediments from Antarctica to the coast.
Photo Credit: Dr Kate Winter, Northumbria University

Research involving scientists from Newcastle University has revealed new hope in natural environmental systems found in Antarctica which could help mitigate the overall rise of carbon dioxide. 

As Antarctica's ice sheets thin due to climate change, newly exposed mountain peaks could significantly increase the supply of vital nutrients to the Southern Ocean which surrounds the continent, potentially enhancing its ability to absorb atmospheric carbon dioxide over long timescales, according to the research published in Nature Communications. 

Led by Northumbria University, a team of scientists looked at analysis of sediment samples from East Antarctica's Sør Rondane Mountains. They discovered that weathered rocks exposed above the ice surface contain iron concentrations up to ten times higher than previously reported from the Antarctic continent. This bioavailable iron is transported to the ocean by glaciers and icebergs, where it fuels the growth of phytoplankton – microscopic marine organisms that absorb CO₂ through photosynthesis. 

Rocks on Faults Can Heal Following Seismic Movement

At the Cascadia subduction zone in the Pacific Northwest, one tectonic plate is moving underneath another. New experimental work at UC Davis shows how rocks on faults deep in the Earth can cement themselves back together after a seismic movement, adding to our knowledge of how these faults behave.
Photo Credit: of Otter Rock, Oregon by USGS

Earthquake faults deep in the Earth can glue themselves back together following a seismic event, according to a new study led by researchers at the University of California, Davis. The work, published in Science Advances and supported by grants from the National Science Foundation, adds a new factor to our understanding of the behavior of faults that can give rise to major earthquakes. 

“We discovered that deep faults can heal themselves within hours,” said Amanda Thomas, professor of earth and planetary sciences at UC Davis and corresponding author on the paper. “This prompts us to reevaluate fault rheological behavior, and if we have been neglecting something very important.” 

Researchers link Antarctic ice loss to ‘storms' at the ocean's subsurface

Mattia Poinelli, a UC Irvine postdoctoral scholar in Earth system science and NASA JPL research affiliate, outlines in a newly published study the impact of submesoscale events – small, subsurface ocean eddies and vortices – on Antarctica’s ice sheets. “Despite being largely overlooked in the context of ice-ocean interactions,” he says, “[they] are among the primary drivers of ice loss.”
Photo Credit: Steve Zylius / UC Irvine

Researchers at the University of California, Irvine and NASA’s Jet Propulsion Laboratory have identified stormlike circulation patterns beneath Antarctic ice shelves that are causing aggressive melting, with major implications for global sea level rise projections.

In a paper published recently in Nature Geoscience, the scientists say their study is the first to examine ocean-induced ice shelf melting events from a weather timescale of just days versus seasonal or annual timeframes. This enabled them to match “ocean storm” activity with intense ice melt at Thwaites Glacier and Pine Island Glacier in the climate change-threatened Amundsen Sea Embayment in West Antarctica.

The research team relied on climate simulation modeling and moored observation tools to gain 200-meter-resolution pictures of submesoscale ocean features between 1 and 10 kilometers across, tiny in the context of the vast ocean and huge slabs of floating ice in Antarctica.

Destination: Mars. First Stop: Iceland?

This picturesque vista is the watershed in southwest Iceland, where researchers collected mars rock analog samples.
Image Credit: Michael Thorpe/NASA Goddard

To say that a trip from Earth to Mars is merely a long one would be a massive understatement. On July 30, 2020, when the National Aeronautics and Space Administration (NASA) sent its Mars rover “Perseverance” atop an Atlas V rocket to the red planet to collect rock samples, it took the rover nearly seven months to reach its destination. This was only one step in a complex process that will take at least a decade to bring home these samples from Mars. While this is an unusually long wait for a sample shipment, it gives scientists ample time to find the best approach to study these rare and precious rocks.

In preparation, an international collaboration of scientists has started investigating sedimentary rock samples found in Iceland, a country whose terrain shares some compositional similarities and whose climate may be similar to ancient climates in certain Martian regions. Their results, published today in American Mineralogist, shed light on how high-resolution analyses of these complex, natural minerals can give scientists a deeper understanding of their geological history, both at home on Earth and 194 million miles away on Mars, though this requires careful interpretation. This collaboration is made up of researchers from the University of Maryland, NASA Goddard, Johnson Space Center, University of Göttingen, Chungbuk National University, and the National Synchrotron Light Source II (NSLS-II), a U.S. Department of Energy (DOE) Office of Science user facility at DOE’s Brookhaven National Laboratory.

Earth Science: In-Depth Description

Image Credit: Scientific Frontline / stock image

Earth Science is the comprehensive study of the planet Earth, encompassing its physical composition, structure, the processes that shape it, and its history. Its primary goal is to understand the complex, integrated systems of our planet—including its solid land (lithosphere), water (hydrosphere), air (atmosphere), and life (biosphere)—and how they interact, change over time, and affect human life.

UC Irvine team track massive ice loss from Berry Glacier in West Antarctica

UC Irvine researchers analyzed decades worth of satellite data to better understand the causes of the rapid retreat of Berry Glacier, a tributary of the Getz Ice Shelf (pictured) in West Antarctica.
Photo Credit: NASA

Berry Glacier, a tributary of the Getz Ice Shelf in West Antarctica, has deteriorated dramatically in the past three decades, according to researchers in the Department of Earth System Science at the University of California, Irvine. In a study published recently in Nature Communications, the scientists documented that in the period spanning 1996 to 2023, the glacier retreated seven-tenths of a kilometer per year for a total of 18 kilometers, about 11 miles. 

Berry Glacier thinned by 11 meters per year during the study period, and its retreat velocity increased by 64 percent, resulting in a loss of 130 gigatons of ice mass. The team derived these results by analyzing synthetic-aperture radar interferometry data from several missions, including ERS-1/2, ALOS-1/2 PALSAR, Sentinel-1, COSMO-SkyMed and the RADARSAT Constellation Mission. 

New study reveals fastest Antarctic glacier retreat in modern history

Hektoria and Green, once glaciated, are now reduced to drifting ice rubble.
Photo Credit: Naomi Ochwat, lead author of the study and Post-Doctoral Associate at CU Boulder’s Cooperative Institute for Research in Environmental Sciences (CIRES), 26 February 2024.

A glacier on the Eastern Antarctic Peninsula has experienced the fastest recorded ice loss in modern history, according to a landmark study co-authored by Swansea University.

Published in Nature Geoscience, the research reveals that Hektoria Glacier lost nearly half its length—eight kilometers of ice—in just two months during 2023; a pace similar to the dramatic retreats seen at the end of the last ice age.

Led by the University of Colorado Boulder, an international team—including Swansea glaciologist, Professor Adrian Luckman—found that Hektoria’s retreat was boosted by the shape of the land beneath it.

Hektoria Glacier rested on an ice plain—a flat stretch of bedrock below sea level—which, once retreat began, saw large sections of ice break away in quick succession.

Six-million-year-old ice discovered in Antarctica offers unprecedented window into a warmer Earth

Raising the Foro Drill, Allan Hills, Antarctica. 2022-2023.
Photo Credit: Julia Marks Peterson, COLDEX.

A team of U.S. scientists has discovered the oldest directly dated ice and air on the planet in the Allan Hills region of East Antarctica.

The 6-million-year-old ice and the tiny air bubbles trapped inside it provide an unprecedented window into Earth’s past climate, according to a new study published today in the Proceedings of the National Academy of Sciences.

The oldest ice sample from Allan Hills dated by researchers clocks in at 6 million years, from a period in Earth’s history where abundant geological evidence indicates much warmer temperatures and higher sea levels compared to today.

Beavers Impact Ecosystems Above and Below Ground

Photo Credit: Gennady Zakharin

Above ground, we can see changes wrought by beaver ponds such as increases in biodiversity and water retention. But UConn Department of Earth Sciences researcher Lijing Wang says we have a limited understanding of how they impact what happens beneath the ground. In research published in Water Resource Research, Wang and co-authors study how water moves through the soils and subsurface environment and detail new insights into how beaver ponds impact groundwater.

Groundwater can be an important source of water for streams, especially late in a dry summer, it may be the only source of water sustaining a stream, says Wang, and researchers are interested in understanding if and how beaver ponds impact groundwater as these details are important to consider for water management and restoration efforts.

Retreating Glaciers May Send Fewer Nutrients to the Ocean

Northwestern Glacier in Alaska has retreated approximately 15 kilometers (nine miles) since 1950.
Photo Credit: Kiefer Forsch/Scripps Institution of Oceanography.

The cloudy, sediment-laden meltwater from glaciers is a key source of nutrients for ocean life, but a new study suggests that as climate change causes many glaciers to shrink and retreat their meltwater may become less nutritious. 

Led by scientists at UC San Diego’s Scripps Institution of Oceanography, the study finds that meltwater from a rapidly retreating Alaskan glacier contained significantly lower concentrations of the types of iron and manganese that can be readily taken up by marine organisms compared to a nearby stable glacier. These metals are scarce in many parts of the ocean including the highly productive Gulf of Alaska, and they are also essential micronutrients for phytoplankton, the microorganisms that form the base of most marine food webs.

Microbes at Red Sea vents show how life and geology shape each other

Microscopic images of the studied microbes.
Image Credit: Courtesy of King Abdullah University of Science and Technology

A new study led by King Abdullah University of Science and Technology (KAUST) Professor Alexandre Rosado has revealed an unusual microbial world in the Hatiba Mons hydrothermal vent fields of the central Red Sea, a site first discovered by one of his co-authors and colleagues, Assistant Professor Froukje M. van der Zwan. 

Published in Environmental Microbiome, the study delivers the first "genome-resolved" analysis of these hydrothermal systems, providing an unprecedented view into both the types of microbes present and the metabolic functions that sustain them. 

“Microbes from the Hatiba Mons fields show remarkable metabolic versatility,” said KAUST Ph.D. student and lead author of the study, Sharifah Altalhi. “By understanding their functions, we can see how life shapes its environment, and how geology and biology are deeply intertwined in the Red Sea.” 

Arctic in Transition: Greenland’s Caves Preserve Ancient Climate Archive

Inside the Cove Cave, northern Greenland: A team of Innsbruck scientists studies deposits from a time when the Arctic was much warmer than today.
Photo Credit: Robbie Shone

In a remote cave in northern Greenland, a research team led by geologists Gina Moseley, Gabriella Koltai, and Jonathan Baker have discovered evidence of a significantly warmer Arctic. The cave deposits show that the region was free of permafrost millions of years ago and responded sensitively to rising temperatures. The findings, published in Nature Geoscience, provide new insights into past climate conditions and their relevance for today’s climate protection efforts.

Understanding Earth’s climate during earlier warm periods is key to predicting how it may change in the future. One particularly revealing time is the Late Miocene, which began about 11 million years ago. During this period, Earth’s distribution of land and ocean was similar to today, and both temperatures and atmospheric CO₂ levels were comparable to projections for the coming decades. Although the Arctic is known to be highly sensitive to climate change, its environmental conditions during the Late Miocene have remained poorly understood.

What Is: Extinction Level Events

A Chronicle of Earth's Biotic Crises and an Assessment of Future Threats
Image Credit: Scientific Frontline

Defining Biotic Catastrophe

The history of life on Earth is a story of breathtaking diversification and innovation, but it is punctuated by chapters of profound crisis. These are the extinction level events—catastrophes of such magnitude that they fundamentally reset the planet's biological clock. Popular imagination often pictures a single, sudden event, like the asteroid that sealed the fate of the dinosaurs. The geological reality, however, is more complex and, in many ways, more instructive for our current era. Understanding these events requires a rigorous scientific framework that moves beyond simple notions of species loss to appreciate the systemic collapse of entire global ecosystems.

New study finds large fluctuations in sea level occurred throughout the last ice age, a significant shift in understanding of past climate

Photo Credit: Michael Chen

Large changes in global sea level, fueled by fluctuations in ice sheet growth and decay, occurred throughout the last ice age, rather than just toward the end of that period, a study published this week in the journal Science has found.

The findings represent a significant change in researchers’ understanding of how the Pleistocene – the geological period from about 2.6 million to 11,700 years ago and commonly known as the last ice age – developed, said Peter Clark Link is external, a paleoclimatologist at Oregon State University and the study’s lead author.

“This is a paradigm shift in our understanding of the history of the ice age,” said Clark, a university distinguished professor in OSU’s College of Earth, Ocean, and Atmospheric Sciences.

During the last ice age, Earth experienced cycles of dramatic shifts in global sea level caused by the formation and melting of large ice sheets over northern areas of North America and Eurasia. These changes are recorded in the shell remains of microscopic marine organisms called foraminifera, which are found in ocean sediment and collected by drilling cores, giving scientists an important record of past climate history.

Geologists discover the first evidence of 4.5-billion-year-old “proto-Earth”

“This is maybe the first direct evidence that we’ve preserved the proto Earth materials,” says Nicole Nie. An artist’s illustration shows a rocky proto Earth bubbling with lava.
Image Credit: MIT News; iStock
(CC BY-NC-ND 4.0)

Scientists at MIT and elsewhere have discovered extremely rare remnants of “proto-Earth,” which formed about 4.5 billion years ago, before a colossal collision irreversibly altered the primitive planet’s composition and produced the Earth as we know today. Their findings, reported today in the journal Nature Geosciences, will help scientists piece together the primordial starting ingredients that forged the early Earth and the rest of the solar system.

Billions of years ago, the early solar system was a swirling disk of gas and dust that eventually clumped and accumulated to form the earliest meteorites, which in turn merged to form the proto-Earth and its neighboring planets.

In this earliest phase, Earth was likely rocky and bubbling with lava. Then, less than 100 million years later, a Mars-sized meteorite slammed into the infant planet in a singular “giant impact” event that completely scrambled and melted the planet’s interior, effectively resetting its chemistry. Whatever original material the proto-Earth was made from was thought to have been altogether transformed.

Earth’s continents stabilized due to furnace-like heat

A new study of the chemical components of rocks led by researchers at Penn State and Columbia University provides the clearest evidence yet for how Earth's continents became and remained so stable — and the key ingredient is heat. 
Photo Credit: Jaydyn Isiminger / Penn State
(CC BY-NC-ND 4.0)

The new discovery has implications beyond geologic history, such as the search for critical minerals and habitable planets beyond Earth

For billions of years, Earth’s continents have remained remarkably stable, forming the foundation for mountains, ecosystems and civilizations. But the secret to their stability has mystified scientists for more than a century. Now, a new study by researchers at Penn State and Columbia University provides the clearest evidence yet for how the landforms became and remained so stable — and the key ingredient is heat. 

In a paper published today (Oct. 13) in the journal Nature Geoscience, the researchers demonstrated that the formation of stable continental crust — the kind that lasts billions of years — required temperatures exceeding 900 degrees Celsius in the planet’s lower continental crust. Such high temperatures, they said, were essential for redistributing radioactive elements like uranium and thorium. The elements generate heat as they decay, so as they moved from the bottom to the top of the crust, they carried heat out with them and allowed the deep crust to cool and strengthen.

Scientists uncover a new way to forecast eruptions at mid-ocean ridges through hydrothermal vent temperatures

Data loggers deployed at hydrothermal vents on the East Pacific Rise record temperature of vent fluids every ten minutes for up to a year.
Photo Credit: Photo courtesy of Jill McDermott, Lehigh Univ.; WHOI, NDSF, Alvin Team; Funder: National Science Foundation. © Woods Hole Oceanographic Institution

A new study provides scientists with a powerful new tool for monitoring and predicting tectonic activity deep beneath the seafloor at mid-ocean ridges—vast underwater mountain chains that form where Earth’s tectonic plates diverge.

The study, titled “Hydrothermal vent temperatures track magmatic inflation and forecast eruptions at the East Pacific Rise, 9°50'N,” reveals that fluctuations in the temperature of fluids flowing from hydrothermal vents occurring over minutes to years indicate the effects of magmatic and tectonic processes that occur miles beneath the seafloor. The research offers the first evidence that these subtle but detectable temperature changes could offer the means to predict seafloor volcanic eruptions.

Led by Thibaut Barreyre of the French National Centre for Scientific Research (CNRS) and University of Brest, with collaborators from Woods Hole Oceanographic Institution (WHOI), Lehigh University, and Scripps Institution of Oceanography, the study presents a 35-year time-series of temperature measurements from five hydrothermal vents along the East Pacific Rise, one of the most active segments and well-studied of the global mid-ocean ridge system.

Understanding volcanoes better

Oldoinyo Lengai in Tanzania is the only active carbonatite volcano on Earth.
Photo Credit: © Miriam Reiss

How do volcanoes work? What happens beneath their surface? What causes the vibrations – known as tremor – that occur when magma or gases move upward through a volcano's conduits? Professor Dr. Miriam Christina Reiss, a volcano seismologist at Johannes Gutenberg University Mainz (JGU), and her team have located such tremor signals at the Oldoinyo Lengai volcano in Tanzania. "We were not only able to detect tremor, but also to determine its exact position in three dimensions – its location and depth below the surface," said Reiss. "What was particularly striking was the diversity of different tremor signals we detected." The findings provide new insights into how magma and gas are transported within the Earth and thus improve our understanding of volcanic dynamics. This also has societal relevance as the researchers hope that their work will enhance the ability to forecast volcanic eruptions in the long term. Their results have recently been published in Communications Earth & Environment.