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Geophysicists at ETH Zurich have shown that every single wave of a magnitude 3.9 earthquake registers in the noise suppression system of fibre-optic networks.

Mars's liquid iron core is smaller and denser than previously thought. Not only is it smaller, but it is also surrounded by a layer of molten rock. This is what researchers conclude on the basis of seismic data from the InSight lander. For four years, NASA's InSight lander recorded tremors on Mars with its seismometer.

Scientists have developed an unprecedented simulation that allows the last 120,000 years of glacier evolution in the Alps to be visualized in 80 seconds.

Biodiversity is greatest in the tropics. That fact that it is hot and humid there plays an important role. However, climate alone cannot explain the global biodiversity patterns well. Researchers at the Swiss Federal Institute for Forest, Snow and Landscape Research have now tackled this old problem from a completely different angle - and identified a new, doubly important reason for high tropical diversity.

An extraordinary heat wave is assailing the world's oceans with an intensity that is surprising climate researchers. Environmental physicist Nicolas Gruber provides some context. Record temperatures in the Mediterranean. Huge heat wave in the North Atlantic. The temperature of the oceans at an all-time high.

A team from the University of Geneva reveals how three easily measurable parameters provide valuable information about the structure of volcanoes. A step forward in risk assessment and preventive measures. What is the risk of a volcano erupting? To answer this question, scientists need information about its underlying internal structure.

With methods of so-called geoengineering, the climate could theoretically be artificially influenced and cooled. Bernese researchers have now investigated whether it would be possible to prevent the melting of the West Antarctic ice sheet by artificially "dimming the sun". The results show that artificial influence does not work without decarbonization and entails high risks.

Alexander von Humboldt was a pioneer of climate research. On his voyages to America (1799-1804) and Asia (1829), he conducted meteorological measurements that he used to develop a modern, holistic model of the Earth's climate.

Scientists have developed a model that sheds light on the seismic risks arising from subsurface fluid injections carried out as part of geothermal energy extraction. To support the shift to a carbon-free economy, energy producers are eagerly looking for ways to safely extract geothermal energy from deep underground.

Researchers have found that droughts and land water variability have had increasing effect on the carbon cycle in the tropics over the last sixty years. Most climate models fail to capture this observation. This could mean that terrestrial ecosystems could absorb less CO2 than expected in their role as carbon sinks in the future.

A strong quake in the last year of the NASA Mars InSight mission, enabled researchers at ETH Zurich to determine the global thickness and density of the planet's crust. On average, the Martian crust much thicker than the Earth's or the Moon's crust and the planet's main source of heat is radioactive.

Bad news for Swiss agriculture: several species of insect pests would find an advantage if the climate continues to warm up.

SLF-scientists Joel Caduff and Yves Bühler trained scientists and practitioners in drone-based snow depth mapping in the Kyrgyz mountains. After packing a lot of equipment including ski touring sets and an eBee-X drone, we boarded the plane to Istanbul on March 29 and then to Biskek, the capital of Kyrgyzstan.

By analysing medieval texts, an international team led by the University of Geneva has succeeded in precisely dating some of the largest eruptions in history. By observing the night sky, medieval monks unwittingly recorded some of history's largest volcanic eruptions. An international team of researchers, led by the University of Geneva , drew on readings of 12th and 13th century European and Middle Eastern chronicles, along with ice core and tree ring data, to accurately date some of the biggest volcanic eruptions the world has ever seen.

A study by the University of Bern concludes that at the end of the last ice age there was not, as previously assumed, a complete collapse of the ocean circulation in the Atlantic, which provide a mild climate in Europe. This realization has implications for the discussion on climate tipping points. The climate does not change linearly.

A new analysis has found rapidly increasing emissions between 2010 and 2020 of five ozone-depleting chemicals whose production for most uses had been banned under the Montreal Protocol. The emissions of these five chlorofluorocarbons, or CFCs, occur in part from leakage during the synthesis of ozone-friendly alternatives to CFCs.

In the Forest Laboratory "Waldlabor" on Hönggerberg, researchers investigate the storage and transport processes of water in the forest. Recently they showed that forest-floor litter and deadwood have a far larger influence on the forest water balance than expected. The forest on Hönggerberg in the north of Zurich is both, a recreational space and a laboratory.

Researchers have studied Vernier, a city in the canton of Geneva, as the pilot site for an interactive map that explores our relationship with the built and natural environments. "Vernier is an odd place. You pass by oil storage tanks, an Ikea, and an airport - and then suddenly you're walking by cows, the Rhône, and little boats." That's how one resident describes what he sees on his daily walking commute.

Forest soils store large amounts of organic carbon. When storms devastate the forest, this carbon is lost and a large part enters the atmosphere as CO2. Mountain forests are particularly vulnerable to such carbon losses, shows a study by the Swiss Federal Institute for Forest, Snow and Landscape Research WSL.

By analysing sediments dating back to the global warming that happened 56 million years ago, a team from the University of Geneva is taking a new look at our climate future. PETM was marked by an increase in the seasonality and intensity of rainfall. This increased the mobility of river channels - the deepest areas of a river - and resulted in the transport of large quantities of fluvial clays deposited on adjacent alluvial plains to the deep ocean.