
A NOAA research vessel trapped in sea ice near Alaska. Increasingly mobile sea ice is a growing hazard for the shipping industry as climate change enables boats to use the Chukchi Sea as a new, faster route between Europe, Asia, and North America. Credit: Crew and Officers of NOAA Ship MILLER FREEMAN
Featured Research
Ship-stranding Arctic ice was forecastable — and will strike again
With 80 more ice-free days per year today than in 1979, the Arctic’s Chukchi Sea is attracting attention as a potential faster route for intercontinental shipping. Climate change has made the sea ice there thinner, allowing boats to pass more easily, but also more mobile as a result, raising the risk of sinking and stranding — as the crew of the Norseman II discovered when three- to five-foot-thick ice trapped them for two weeks in 2024. A new study found that the sudden influx of windblown ice that stranded the Norseman II could have been predicted using satellite imagery, weather data, and simulations of ice and ocean movement. With more vessels set to navigate this changing sea in the coming years, the study’s authors recommend that researchers collaborate with ship operators to communicate ice hazard forecasts. [Geophysical Research Letters study]
Lightning strikes scramble rocks’ magnetic signatures
Electrocuting volcanic rocks with a lightning-like current can make them up to 490 times more magnetic, according to a new study. When volcanic rocks form, some iron-rich minerals interact with Earth’s magnetic field as they crystallize from lava or magma, locking in a magnetic fingerprint. Lightning can deliver a current of 80,000 amps — 6,400 times what’s needed to run a high-power blender. This generates a combined magnetic field and heat pulse, short-lived but strong enough to scramble rocks’ magnetic signatures and even create entirely new, microscopic, magnetic minerals. Researchers suggest zapping rocks in the lab can help geologists identify lightning-affected rocks to not only find signs of past storms but also interpret the magnetic fingerprint to tell where rocks formed. [JGR Solid Earth study]
Listening for wildfires with infrasound
Wildfires generate low-pitched sound imperceptible to humans but audible to infrasound detectors from as far as 1.8 miles (3 kilometers) away. A new study deployed arrays of sensors to listen for planned sagebrush fires and found that the sound of burning vegetation can be used to locate and track fires as they progress. This works even when the fire is more a smolder than a blaze and with as few as three infrasound detectors, although using more detectors allowed researchers to track fires from further away. Unlike satellite- and aircraft-based sensors, infrasound detectors can monitor continuously over large areas at low cost without being affected by smoke or tree cover, making them valuable to future fire monitoring, researchers say. [Geophysical Research Letters study]
Algae sought sanctuary in dark dirt on Snowball Earth
A new study finds that prehistoric algae could have survived average temperatures as low as -60 degrees Celsius (-76 F) by clustering on patches of dark land, potentially explaining how photosynthetic organisms withstood Earth’s ‘snowball’ phases 600 million years ago. Earth has had at least two snowball periods when low atmospheric carbon dioxide and a dimmer sun created such cold conditions that almost the entire planet froze over. Researchers calculate that darker areas of remaining bare land absorbed just enough heat from the sun to melt any ice that crept into them from snowfall or the edges of glaciers. These snowmelt sanctuaries could have covered between 0.1% and 12% of the Earth, creating a way for algae to eke out an existence. [JGR Atmospheres study]
Mapping the hidden landscape beneath Greenland’s ice
Researchers have peered through Greenland’s ice sheet to reveal a hidden landscape which records at least two million years of the island’s glacial history. Using satellite observations and measurements from the surface, a new study extrapolated lumps and bumps at the top of the ice to map out a vast network of frozen valleys and mountain ranges in the bedrock below. The map is so detailed that it’s possible to distinguish different rock formations through patterns in the valleys under the ice, as well as the now ice-covered mountains where Greenland’s modern ice sheet likely started to form. [Geophysical Research Letters study]
What Australian lakes showed us about Martian hydrology
Studying the hydrology of the Yilgarn Craton reveals how the Red Planet may have evolved. [Eos research spotlight] [Earth and Space Science study]
Redesigning farmland through community collaboration in California
A community-led project in California shows how collaboration can reshape farmland to improve water resources, restore native plants, and create recreational space. [Eos editors’ highlight] [Community Science study]








