Results 31 to 40 of about 147,239 (238)

Finding antipodal point grasps on irregularly shaped objects [PDF]

open access: yes, 1992
Two-finger antipodal point grasping of arbitrarily shaped smooth 2-D and 3-D objects is considered. An object function is introduced that maps a finger contact space to the object surface. Conditions are developed to identify the feasible grasping region,
Burdick, Joel W., Chen, I-Ming
core   +2 more sources

Spatiospectral concentration of vector fields on a sphere [PDF]

open access: yes, 2013
We construct spherical vector bases that are bandlimited and spatially concentrated, or, alternatively, spacelimited and spectrally concentrated, suitable for the analysis and representation of real-valued vector fields on the surface of the unit sphere,
Plattner, Alain, Simons, Frederik J.
core   +1 more source

Dimension-Free Estimates for the Discrete Spherical Maximal Functions

open access: yesInternational Mathematics Research Notices, 2023
Abstract We prove that the discrete spherical maximal functions (in the spirit of Magyar, Stein, and Wainger) corresponding to the Euclidean spheres in $\mathbb {Z}^{d}$ with dyadic radii have $\ell ^{p}(\mathbb {Z}^{d})$ bounds for all $p\in [2, \infty ]$ independent of the dimensions $d\ge 5$.
Mirek, M., Szarek, T.Z., Wróbel, B.
openaire   +4 more sources

An Lp−Lq version of Hardy's theorem for spherical Fourier transform on semisimple Lie groups

open access: yesInternational Journal of Mathematics and Mathematical Sciences, 2004
We consider a real semisimple Lie group G with finite center and K a maximal compact subgroup of G. We prove an Lp−Lq version of Hardy's theorem for the spherical Fourier transform on G.
S. Ben Farah, K. Mokni, K. Trimèche
doaj   +1 more source

On the unramified spectrum of spherical varieties over p-adic fields [PDF]

open access: yes, 2008
The description of irreducible representations of a group G can be seen as a question in harmonic analysis; namely, decomposing a suitable space of functions on G into irreducibles for the action of G x G by left and right multiplication. For a split p-
Sakellaridis, Yiannis
core   +2 more sources

Sparse bounds for spherical maximal functions [PDF]

open access: yesJournal d'Analyse Mathématique, 2019
We consider the averages of a function $ f$ on $ \mathbb R ^{n}$ over spheres of radius $ 0< r< \infty $ given by $ A_{r} f (x) = \int_{\mathbb S ^{n-1}} f (x-r y) \; d (y)$, where $ $ is the normalized rotation invariant measure on $ \mathbb S ^{n-1}$.
openaire   +2 more sources

Development of a new hybrid approach combining AFM and SEM for the nanoparticle dimensional metrology

open access: yesBeilstein Journal of Nanotechnology, 2019
At this time, there is no instrument capable of measuring a nano-object along the three spatial dimensions with a controlled uncertainty. The combination of several instruments is thus necessary to metrologically characterize the dimensional properties ...
Loïc Crouzier   +9 more
doaj   +1 more source

On families between the Hardy–Littlewood and spherical maximal functions [PDF]

open access: yesArkiv för Matematik, 2021
We study a family of maximal operators that provides a continuous link connecting the Hardy-Littlewood maximal function to the spherical maximal function. Our theorems are proved in the multilinear setting but may contain new results even in the linear case.
Georgios Dosidis, Loukas Grafakos
openaire   +1 more source

Lacunary Discrete Spherical Maximal Functions

open access: yes, 2018
We prove new $\ell ^{p} (\mathbb Z ^{d})$ bounds for discrete spherical averages in dimensions $ d \geq 5$. We focus on the case of lacunary radii, first for general lacunary radii, and then for certain kinds of highly composite choices of radii.
Kesler, Robert   +2 more
openaire   +3 more sources

Earth crust vertical movements according to ITRF2000, ITRF2005, ITRF2008 and ITRF2014 coordinate systems and their comparing analysis

open access: yesGeodesy and Geodynamics, 2018
The analysis of Earth’s crust movement vertical velocities was made both for separate regions, and averaged on regions. As input data coordinates and velocities of earth crust points, obtained in International Coordinate Systems ITRF2000, ITRF2005 ...
N.A. Chujkova   +3 more
doaj   +1 more source

Home - About - Disclaimer - Privacy