Results 221 to 230 of about 26,118 (326)
Doubling of Asymptotically Flat Half-spaces and the Riemannian Penrose Inequality. [PDF]
Commun Math Phys, 2023 Eichmair M, Koerber T.
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Homotopy groups, focal points, and totally geodesic immersions [PDF]
, 2013 Sérgio Mendonça, Heudson Mirandola
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Journal of Geophysical Research: Solid Earth, Volume 131, Issue 6, June 2026.Abstract The physical mechanisms that govern the multi‐scale source properties of earthquakes, such as fracture energy scaling, where the dynamic energy dissipation of earthquakes scales with fault slip, remain debatable. We introduced the rate‐ and roughness‐dependent friction (RRF) law which accounts for the multi‐scale roughness evolution of the ...
Reiju Norisugi, Hiroyuki Noda
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Anomalous Geodesics in the Inhomogeneous Corner Growth Model. [PDF]
Commun Math PhysEmrah E, Janjigian C, Seppäläinen T.
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Towards Unification of General Relativity and Quantum Theory: Dendrogram Representation of the Event-Universe. [PDF]
Entropy (Basel), 2022 Shor O, Benninger F, Khrennikov A.
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A bound on the dimension of a totally geodesic submanifold in the Prym locus [PDF]
, 2019 Colombo, E.
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A Deep Ensemble Transformer Model for Global Ionosphere Prediction and Uncertainty Quantification
Journal of Geophysical Research: Machine Learning and Computation, Volume 3, Issue 3, June 2026.Abstract Accurate global ionospheric forecasting is important for various purposes, from geophysical research to practical applications, including real‐time precise positioning and navigation. Existing studies primarily focus solely on deterministic predictions and often overlook uncertainty quantification.
Shuyin Mao, Junyang Gou, Benedikt Soja
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Geometric Bounds for Low Steklov Eigenvalues of Finite Volume Hyperbolic Surfaces. [PDF]
J Geom AnalHassannezhad A, Métras A, Perrin H.
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Arc Heat Flow and Magmatic Heat Budgets
Reviews of Geophysics, Volume 64, Issue 2, June 2026.Abstract We evaluate hydrothermal heat loss from 11 volcanic‐arc segments (∼6,000 km of arc length, ∼10% of the global total), motivated by the observation that much magmatic heat ultimately crosses the land surface as heated aqueous fluid. Heat loss takes place by volcanic eruption, geothermal heat conduction to the surface, fumarolic (vapor ...
S. E. Ingebritsen +7 more
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