Results 111 to 120 of about 715 (188)
GEODESIC VECTORS ON $5$-DIMENSIONAL HOMOGENEOUS NILMANIFOLDS
Summary: In this paper, firstly we study geodesic vectors for the \(m\)-th root homogeneous Finsler space admitting \((\alpha,\beta)\)-type. Then we obtain the necessary and sufficient condition for an arbitrary non-zero vector to be a geodesic vector for the \(m\)-th root homogeneous Finsler metric under mild conditions. Finally, we consider a quartic
Shanker, Gauree +2 more
openaire +2 more sources
Integrable geodesic flows of Riemannian and sub-Riemannian metrics on Lie groups and homogeneous spaces [PDF]
We discuss general algebraic methods for constructing integrable geodesic flows of Riemannian and sub-Riemannian metrics on homogeneous spaces and Lie groups. Our approach is based on the concept of non-commutative integrability and the classical idea of
Alexey Bolsinov (1258812)
core
Abstract Relative plate motion in subduction zones transitions from frictional slip to viscous flow with increasing depth and temperature. The frictional‐viscous transition can control the depth extent of megathrust earthquakes and episodic tremor and slip (ETS).
So Ozawa +2 more
wiley +1 more source
A note on geodesic and almost geodesic mappings of homogeneous Riemannian manifolds
Tyt. z nagł.Abstract. Let M be a differentiable manifold and denote by nabla and nabla~ two linear connections on M. Nabla and nabla~ are said to be geodesically equivalent if and only if they have the same geodesics.
Formella, Stanisław.
core
Homogeneous geodesics of non-reductive homogeneous pseudo-Riemannian 4-manifolds
After obtaining an explicit description in global coordinates of invariant metrics on four-dimensional non-reductive homogeneous pseudo-Riemannian manifolds, for each of these spaces we completely describe Killing and geodesic vector elds and ...
Giovanni Calvaruso +5 more
core +1 more source
Abstract The seismic behavior of subduction megathrusts varies spatially and is influenced by the properties of subducting plates, including their sedimentary cover. Characterizing these subduction inputs is essential for understanding the mechanisms behind fault slip variability.
Philip M. Barnes +12 more
wiley +1 more source
Importance of Spatially Continuous Urban Surface Properties in Urban‐Resolving Earth System Modeling
Abstract Accurate representation of urban properties and processes at higher resolutions in global modeling systems is essential for advancing our ability to capture the complexities of urban systems and informing effective resilience strategies. However, the prescription of coarse global‐scale urban properties in most state‐of‐the‐art Earth system ...
Yifan Cheng +6 more
wiley +1 more source
Arc Heat Flow and Magmatic Heat Budgets
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
wiley +1 more source
Differing Manifestations of Spatial Curvature in Cosmological FRW Models
We found statistical evidence for a mismatch between the (global) spatial curvature parameter K in the geodesic equation for incoming photons and the corresponding parameter in the Friedmann equation that determines the time evolution of the background ...
Meir Shimon, Yoel Rephaeli
doaj +1 more source
Two‐Layer Anisotropy Beneath Subduction Zones: Bayesian Inversion
Abstract Shear‐wave splitting measurements have the potential to constrain multiple layers of anisotropy and thereby enhance depth resolution. Using the formulation of Silver and Savage (1994, https://doi.org/10.1111/j.1365‐246x.1994.tb04027.x), previous studies have employed deterministic grid‐search approaches to identify best‐fitting two‐layer ...
Cheng‐Chien Peng +2 more
wiley +1 more source

