Results 211 to 220 of about 42,838 (280)
Assessment of Physical Properties and Potential Elemental Leaching from Bauxite Tailing-Based Alkali-Activated Materials. [PDF]
Barreto IAR, da Costa ML.
europepmc +1 more source
Abstract Springtime warming over Northern Mid‐High‐latitude Land profoundly affects plant life cycles and water resources, yet large model uncertainty limits climate risk assessment. Here, we develop a novel emergent constraint that targets the key uncertainty source—model divergence in surface‐albedo feedback linked to historical snowmelt sensitivity.
Shuzhen Hu +4 more
wiley +1 more source
A High Spatial and Depth Resolution Deep-UV 266 nm Wavelength Laser-Based Integrated LIBS, Fluorescence, and Raman System for Probing Lunar and Planetary Simulants and Geological Materials. [PDF]
Aryal A +7 more
europepmc +1 more source
Abstract Reconstructing oroclinal orogens along the Fuegian Andes‐northern Antarctic Peninsula provides critical constraints on the pre‐opening tectonic evolution of the Drake Passage, although such efforts are limited by a lack of reliable Cretaceous paleomagnetic and geochronological data.
Liang Gao +6 more
wiley +1 more source
Siderite and ferric oxyhydroxides imply interlinked carbon, iron, and halogen cycles on Mars. [PDF]
Mitra K +3 more
europepmc +1 more source
AMOC Weakening Shapes Ocean Heat Storage Patterns Under Strong Idealized Warming
Abstract The ocean absorbs most of the excess heat induced by anthropogenic greenhouse gas emissions. Among the different processes, a key role has been attributed to the Atlantic Meridional Overturning Circulation (AMOC), both for heat uptake and redistribution among basins, yet a comprehensive view remains elusive. In this study, we investigate how a
Chiara Ventrucci +4 more
wiley +1 more source
The glass-ceiling convective regime and the origin and diversity of coronae on Venus. [PDF]
Kerr MC +3 more
europepmc +1 more source
How Unusual Was the Paleocene‐Eocene Thermal Maximum?
Abstract The Paleocene‐Eocene Thermal Maximum (PETM) was an extreme fluctuation of Earth's climate and a potential analog for future unmitigated anthropogenic climate change, but whose cause is debated. We show that fluctuations in Cenozoic benthic foraminiferal δ13 ${\delta }^{13}$C and δ18 ${\delta }^{18}$O follow a Laplace distribution. We present a
B. B. Cael, G. L. Foster
wiley +1 more source
Hydrothermal alteration of Ryugu from a disruptive impact recorded in a returned sample. [PDF]
Schrader DL +3 more
europepmc +1 more source

