Results 221 to 230 of about 94,825 (311)
Abstract Permafrost degradation under a warming climate has altered hydrological and biogeochemical processes across the Arctic. Although increasing fluxes of weathering‐derived ions (e.g., Ca2+, Mg2+, and SO42−) have been reported in Arctic rivers, the underlying mechanisms and hotspots within basins remain poorly understood due to limited analysis of
Y. Tashiro +10 more
wiley +1 more source
Keep palm and carry on: Limited role of thermal acclimation in the invasion of a palm species in Central Europe. [PDF]
Gauthey A.
europepmc +1 more source
Magma Storage Below Sabancaya Volcano (Southern Peru) Imaged by Broadband Magnetotellurics
Abstract Sabancaya volcano is one of the most active volcanoes in the Central Andes. Its ongoing eruptive process is accompanied by large‐scale deformation, with activation of the Huambo‐Cabanaconde fault system, marked by intense seismicity over an area of about 50 × 30 km2 ${\mathrm{k}\mathrm{m}}^{2}$.
Jose‐Luis Torres +11 more
wiley +1 more source
Abstract Constraints on three‐dimensional fault system geometry and kinematics are required to understand both long‐term tectonics and contemporary seismic hazard. In many cases, these parameters must be inferred from a combination of different data or analyses.
A. M. Mere +3 more
wiley +1 more source
Binary classification of signal and background triggers of a transition edge sensor using convolutional neural networks. [PDF]
Rivasto E +7 more
europepmc +1 more source
Abstract Central to our understanding of mantle convection and inner Earth material transport is the mantle transition zone. Mantle transition zone thicknesses can reveal key constraints on the locations and degree of material transport between the upper mantle and lower mantle.
Yuhang Dai +2 more
wiley +1 more source
Glymphatic system dysfunction correlated with gut dysbiosis and cognitive impairment in schizophrenia. [PDF]
Wu H +7 more
europepmc +1 more source
Mantle Transition Zone Topography in New Zealand From Teleseismic P $P$‐Wave Receiver Functions
Abstract The geology of New Zealand has been shaped by tectonic plate interactions driven by mantle convection over the past 60 million years, but the effects of these interactions on the transition to the lower mantle are not yet well understood. We analyze 10 years of teleseismic P $P$‐wave receiver functions using common conversion point stacking to
Quan Zhang +4 more
wiley +1 more source
DTI-ALPS index as a predictor of glymphatic system dysfunction in cerebral infarction. [PDF]
Lin B, Leong YY, Mohamad M.
europepmc +1 more source

