Results 111 to 120 of about 639 (201)

Riemannian L-systems: modelling growing forms in curved spaces. [PDF]

Quant Plant Biol
Godin C, Boudon F.
europepmc   +1 more source

Air‐Sea Momentum Exchange With Explicit Wind‐Wave‐Current Coupling and Effects on Hurricane Structure and Impacts

Earth and Space Science, Volume 13, Issue 8, August 2026.
Abstract Ocean surface waves play an essential role in momentum exchange between the atmosphere and ocean, which is especially important in tropical cyclones. A key coupling process that is often omitted by coupled models using bulk or simplified stress parameterizations is the explicit representation of wind‐wave and wave‐ocean vector stresses.
Alton P. Daley, Shuyi S. Chen
wiley   +1 more source

Ray Transform of Symmetric Tensor Fields on Riemannian Manifolds with Conjugate Points. [PDF]

J Geom Anal
Holman S, Krishnan VP.
europepmc   +1 more source

Crustal Thickness Inversion From Magmatic Geochemistry Reveals Spatiotemporal Evolution and Two‐Stage Uplift of the Iranian Plateau

Geochemistry, Geophysics, Geosystems, Volume 27, Issue 8, August 2026.
Abstract The Cenozoic topographic growth of the Iranian Plateau, situated at the Arabia‐Eurasia collision front, provides insights into continental collision dynamics. However, the relative contributions of tectonic shortening versus deep mantle processes to crustal thickening remain debated because systematic quantitative constraints on paleo‐crustal ...
Jun Hu, Yongwei Zhao, Zhengquan Chen, Ni Li, Huan Kang   +4 more
wiley   +1 more source

Minimum Spacetime Length and the Thermodynamics of Spacetime. [PDF]

Entropy (Basel)
Rossi V, Cacciatori SL, Pesci A.
europepmc   +1 more source

Impact of Heterogeneous Mantle Viscosity on the Glacial Isostatic Adjustment Correction for GRACE(‐FO): Implications for Surface Mass Trends

Journal of Geophysical Research: Solid Earth, Volume 131, Issue 8, August 2026.
Abstract Accurate interpretation of time‐variable gravity from GRACE (‐FO) requires correction for glacial isostatic adjustment (GIA), which has a gravitational signal similar in magnitude to that of contemporary hydrological and cryospheric mass change.
E. Hightower, L. Caron, F. Landerer, M. Watkins, E. Ivins, E. Larour   +5 more
wiley   +1 more source

Walks with jumps: a neurobiologically motivated class of paths in the hyperbolic plane. [PDF]

J Math Biol
DeBlois J, Einstein E, Victor JD.
europepmc   +1 more source

Improving Earthquake Forecasting for Europe Using Elliptic ETAS Aftershock Distribution Kernels

Journal of Geophysical Research: Solid Earth, Volume 131, Issue 8, August 2026.
Abstract In the standard Epidemic‐Type Aftershock Sequence (ETAS) model, widely used for earthquake forecasting, aftershocks are distributed isotropically in space—in circular symmetry around the triggering event. This simplification neglects fault geometry and observed anisotropy in aftershock distributions.
M. Han, L. Mizrahi, S. Wiemer
wiley   +1 more source

Ionized Keplerian Disks Demonstrating Interplay Between Strong Gravity and Magnetism. [PDF]

Entropy (Basel)
Stuchlík Z, Vrba J.
europepmc   +1 more source

Dynamic Evolution of Forearc Subsidence Controlled by Slab Geometry

Journal of Geophysical Research: Solid Earth, Volume 131, Issue 8, August 2026.
Abstract Several subduction zones worldwide present an enigmatic forearc topography and strain characterized by extension at a forearc ridge near the trench and shortening within a forearc valley located between the ridge and the magmatic arc. The development of this topography has been linked to progressive slab steepening, while strain patterns ...
F. Bolrão, W. P. Schellart
wiley   +1 more source