Tectonic origins of the Great Unconformity

In 1869, geologist John Wesley Powell made a startling discovery while exploring the Grand Canyon: a 520-million-year-old rock layer resting directly atop rocks 1.4 to 1.8 billion years old. Nearly a billion years of geological history appeared to be missing. This vast temporal gap, now known as the Great Unconformity, is not unique to the …

The power of climate models explained

Weather forecasts and long-term climate projections may seem almost magical, but they rest on decades of scientific and computational advances. The Earth system is an intricate network of interacting components: oceans circulate heat across basins, forests exchange carbon with the atmosphere, storms redistribute moisture and energy, and human activities alter atmospheric composition. All of these …

The growing gravity anomaly under Antarctica

Earth may appear nearly spherical, but its gravitational field tells a different story. Instead of a smooth shell, Earth’s gravity resembles a lumpy potato, shaped by uneven mass distribution deep inside the planet. One of the most striking features of this distorted field is the Antarctic Geoid Low—a broad depression beneath Antarctica where gravity is …

AI vs physics in cloud feedback uncertainty

In 2008, atmospheric scientist Chris Bretherton flew through clouds above the Atacama Desert aboard an instrument-packed C-130 aircraft, gathering data on ice, water vapor, and air pressure. His goal was not sightseeing but confronting one of climate science’s hardest problems: understanding clouds. Nearly two decades later, as global temperatures have risen by about half a …

Geomagnetic reversals lasted far longer than thought

Earth’s magnetic field is generated by the turbulent motion of molten nickel and iron in the planet’s outer core. Although this invisible shield feels permanent, it periodically weakens and reorganizes, causing the magnetic north and south poles to swap places. These events, known as Geomagnetic reversals, are recorded in rocks and ocean sediments, where tiny …

Snowball Earth was frozen, not static

Scientists from University of Southampton have uncovered remarkable new evidence showing that Earth’s climate did not completely shut down during its most extreme ice age, Snowball Earth. This period occurred in the Cryogenian, roughly 720–635 million years ago, when ice sheets stretched to the tropics and the planet may have appeared fully frozen from space. …