The Eta Aquarids meteor shower, ongoing since late April, reaches its peak during the first week of the month. During the early-morning hours of May 5 and 6, up to dozens of meteors per hour will streak through the sky in the best viewing locations.
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Over the past decades, many countries worldwide have been trying to gradually transform their energy systems, with the aim of reducing carbon emissions and mitigating the adverse effects of climate change. Hydrogen and carbon dioxide (CO2) transport networks, infrastructures designed to transport hydrogen gas and captured CO2, could support the shift towards climate-neutral energy systems.
Researchers at Technical University Berlin carried out a study aimed at better understanding the extent to which hydrogen and CO2 transport networks could contribute to the future de-carbonization of the European energy system. Their paper, published in Nature Energy, suggests that both these types of networks could play a key role in establishing a sustainable and clean European energy system.
“In our view, we are envisioning a climate-friendly economy which relies as little as possible on fossil fuels and respects socio-economic considerations,” Fabian Hofmann, first author of the paper, told Tech Xplore.
To combat climate change and achieve a climate-neutral industry, carbon emissions must be drastically reduced. A key part of this transition is replacing carbon-based energy carriers with electricity, particularly in transport and industrial applications. However, this shift heavily depends on nickel, a critical material used in batteries and stainless steel.
Comets that have hit Earth have been a mixed bag. Early in Earth’s history, during the solar system’s chaotic beginning, they were likely the source of our planet’s water, ultimately making up about 0.02% of the planet’s mass. (Mars and Venus received a similar fraction.)
Comets brought complex organic molecules and the biosphere, but later posed a threat to the same in cometary collisions. A comet (or asteroid) likely caused the Tunguska Event in 1908 in Russia, and a comet fragment likely triggered the rapid climate shift of the Younger Dryas 12,800 years ago, with its widespread extinctions.
If such collisions happen here, they likely take place in other solar systems as well. Now three scientists in the United Kingdom have modeled the impacts of an icy cometary collision with an Earth-like, tidally locked terrestrial planet. Such objects are prime candidates in the search for habitable exoplanets outside our solar system.
The European Space Agency’s seventh Earth Explorer mission, Biomass, launched on Tuesday aboard an Arianespace Vega-C rocket. Biomass, which will study Earth’s forests and their impact on the planet’s climate, lifted off from Kourou, French Guiana, at 09:15 UTC (6:15 AM local time).
Durham University has contributed to new international research that critically assesses the intricate relationship between urban digitization and sustainability, focusing on the significant environmental impact of data centers.
Scientists at the University of California, Berkeley, and Boise State University have found evidence suggesting that the Marinoan glaciation began approximately 639 million years ago and lasted for approximately 4 million years. In their study published in the Proceedings of the National Academy of Sciences, the group used drone and field imagery along with isotopic dating of glacial deposits to learn more about global glaciation events during the Neoproterozoic Era.
Prior research has shown that during the early days of the planet, during the Neoproterozoic Era, Earth underwent two ice ages. The first, known as the Sturtian glaciation, lasted approximately 56 million years and covered the entire planet with ice. Less is known about the second event, called the Marinoan glaciation. In this new effort, the research team set themselves the task of figuring out when it began and how long it lasted.
The work involved sending drones over a part of Namibia, where prior research has uncovered evidence of glacial activity during the Marinoan. This allowed the team to map sedimentary layers that were stacked up in a way that showed little vertical shift had occurred, which meant the glaciers did not move much during the time they were there. Additional field imagery helped confirm what the team found in the drone images.
Criegee intermediates (CIs)—highly reactive species formed when ozone reacts with alkenes in the atmosphere—play a crucial role in generating hydroxyl radicals (the atmosphere’s “cleansing agents”) and aerosols that impact climate and air quality. The syn-CH3CHOO is particularly important among these intermediates, accounting for 25%–79% of all CIs depending on the season.
Until now, scientists have believed that syn-CH3CHOO primarily disappeared through self-decomposition. However, in a study published in Nature Chemistry, a team led by Profs. Yang Xueming, Zhang Donghui, Dong Wenrui and Fu Bina from the Dalian Institute of Chemical Physics (DICP) of the Chinese Academy of Sciences has uncovered a surprising new pathway: syn-CH3CHOO’s reaction with atmospheric water vapor is approximately 100 times faster than previously predicted by theoretical models.
Using advanced laser techniques, the researchers experimentally measured the reaction rate between syn-CH3CHOO and water vapor, and discovered the faster reaction time. To uncover the reason behind this acceleration, they constructed a high-accuracy full-dimensional (27D) potential energy surface using the fundamental invariant-neural network approach and performed full-dimensional dynamical calculations.
Over 100 red sprites were captured above the Himalayas in 2022. A study linked them to strong lightning strikes in a large thunderstorm system and introduced a new timing method for analysis. Have you ever heard of or seen red lightning? These are not animated characters, but real atmospheric ph
The system, designed to enhance protection for critical infrastructures, has proven its ability to withstand the immense force of lightning strikes while maintaining stable flight.
