Under current climate policies, 79 per cent of the world’s glaciers will disappear by 2100, endangering the water supply for 2 billion people and raising sea levels dramatically
A climate study led by The Hong Kong University of Science and Technology (HKUST), in collaboration with an international research team, reveals that under a high-emission scenario, the Northern Hemisphere summer monsoons region will undergo extreme weather events starting in 2064. Asia and broader tropical regions will face frequent “subseasonal whiplash” events, characterized by extreme downpours and dry spells alternating every 30 to 90 days which trigger climate disruptions with catastrophic impacts on food production, water management, and clean energy systems.
Published in Science Advances under the title “Increased Global Subseasonal Whiplash by Future BSISO Behavior,” the research was co-led by Prof. Lu Mengqian, Director of the Otto Poon Center for Climate Resilience and Sustainability and Associate Professor of the Department of Civil and Environmental at HKUST and Dr. Cheng Tat-Fan, a postdoctoral fellow in the Department of Civil and Environmental Engineering at HKUST, alongside collaborators from the University of Hawaiʻi at Mānoa, Sun Yat-Sen University and Nanjing University of Information Science and Technology.
About 50,000 years ago, humanity lost one of its last surviving hominin cousins, Homo floresiensis (also known as “the hobbit” thanks to its small stature). The cause of its disappearance, after more than a million years living on the isolated volcanic island of Flores, Indonesia, has been a longstanding mystery.
Now, new evidence suggests a period of extreme drought starting about 61,000 years ago may have contributed to the hobbits’ disappearance.
Our new study, published today in Communications Earth & Environment, reveals a story of ecological boom and bust. We’ve compiled the most detailed climate record to date for the site where these ancient hominins once lived.
The building sector accounts for nearly 40% of global energy consumption and over one-third of energy-related carbon emissions. Therefore, it is vital to adopt low-carbon design strategies. Double-Skin Façades (DSFs) offer significant potential to improve energy efficiency through the dynamic control of heat and daylight. This study evaluates the combined effects of building orientation, fixed shading devices, and adjustable blinds on the performance of DSFs across six cities representing diverse climate types: Phoenix, Stockholm, Kuala Lumpur, London, Cape Town, and Tokyo. Using a model developed in DesignBuilder, 852 scenarios were simulated with 5-min time steps over a full year. The results show that optimal orientation depends on the climate and that cooling load may be reduced up to 59%, with CO2 emission savings up to 11.7% compared to a base south-facing configuration.
When a gas is highly energized, its electrons get torn from the parent atoms, resulting in a plasma—the oft-forgotten fourth state of matter (along with solid, liquid, and gas). When we think of plasmas, we normally think of extremely hot phenomena such as the sun, lightning, or maybe arc welding, but there are situations in which icy cold particles are associated with plasmas. Images of distant molecular clouds from the James Webb Space Telescope feature such hot–cold interactions, with frozen dust illuminated by pockets of shocked gas and newborn stars.
Now a team of Caltech researchers has managed to recreate such an icy plasma system in the lab. They created a plasma in which electrons and positively charged ions exist between ultracold electrodes within a mostly neutral gas environment, injected water vapor, and then watched as tiny ice grains spontaneously formed.
They studied the behavior of the grains using a camera with a long-distance microscope lens. The team was surprised to find that extremely “fluffy” grains developed under these conditions and grew into fractal shapes—branching, irregular structures that are self-similar at various scales. And that structure leads to some unexpected physics.
A new study led by researchers from the Institute of Atmospheric Physics of the Chinese Academy of Sciences (CAS) has uncovered the first observational evidence of lateral negative re-discharges occurring on negative leader channels. Published recently in Geophysical Research Letters, the findings offer new insights into how lightning channels remain electrically active and how their structures evolve before and after a return stroke.
Prior to this research, negative-polarity lateral breakdowns had only been observed near the tips of positive leaders—never documented along negative leader channels.
Dr. Briony Horgan: “You need so much water that we think these could be evidence of an ancient warmer and wetter climate where there was rain falling for millions of years.”
What was Mars like billions of years ago? This is what a recent study published in Communications Earth & Environment hopes to address as an international team of scientists investigated intriguing evidence from the surface of Mars that could indicate heavy water activity existed long ago. This study has the potential to help scientists better understand ancient conditions on Mars and whether they were favorable for supporting life as we know it.
For the study, the researchers examined aluminum-rich rock fragments that were discovered by NASA’s Perseverance rover within Jezero Crater on Mars, and specifically the processes how they formed. This is because aluminum-rich clay minerals on Earth often form from heavy rainfall or other water-driven activities. Using the rover’s SuperCam and Mastcam-Z instruments, the researchers discovered the fragments—which were composed of aluminum and titanium with depleted traces of iron and magnesium—likely were analogs for heavy rainfall on Earth under greenhouse conditions. Therefore, the researchers concluded they potentially formed under intense wet conditions on Mars.
Rocks that stood out as light-colored dots on the reddish-orange surface of Mars now are the latest evidence that areas of the small planet may have once supported wet oases with humid climates and heavy rainfall comparable to tropical climates on Earth.
The rocks discovered by NASA’s Perseverance Mars rover are white, aluminum-rich kaolinite clay, which forms on Earth after rocks and sediment are leached of all other minerals by millions of years of a wet, rainy climate.
These findings were published Monday (Dec. 1) in the journal Communications Earth & Environment by lead author Adrian Broz, a Purdue University postdoctoral research associate in the lab of Briony Horgan, a long-term planner on NASA’s Mars Perseverance rover mission and professor of planetary science in the Department of Earth, Atmospheric, and Planetary Sciences in Purdue’s College of Science.
As artificial intelligence devours electricity, a quiet nuclear revolution is taking shape deep below future data centers.
Across Europe, tech firms are staring at an uncomfortable equation: soaring digital demand, power grids near saturation, and climate goals that leave little room for more fossil fuels. A young French company now claims it can rewrite that equation with a compact reactor that hides underground and feeds on nuclear waste.