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0) (1,u) 6 R(uF(λ, 0)) holds;(H3) uF(λ,u) is a Fredholm operator of index zero whenever F(λ,u) = 0 with (λ,u) O;(H4) for ... It is therefore a Fredholm operator of index zero (see [6, Theorem 2.7.6]).

10 Apr 2011: x2 x8!21 h x!2 h x8! 2,. 6! where the vortex sheet strengthg satisfies a Fredholm integral equation of the second kindg 1 2AmŪ@ g #• 1,hx!

23 Jan 2004: that. ‖K‖ 14 ‖etÃF̃ etÃ‖h2 O(h3).(2.1)Therefore ‖K‖ scales with h2, rather than with h in standard applications ofNeumann expansions to, say, Fredholm equations of the second

is. given by. π(HY ,T) = ind(T),. where ind(T) is the Fredholm index of T.

D. T.-R. McLaughlin, and A. Minakov. Soliton v.the gas: Fredholm determinants, analysis, and the rapid oscillations behind the kineticequation arXiv:2205.02601, 2022.

26 Jul 2013: Eqn (21) is a well-posed. Fredholm integral equation of the second kind for the unknown.

2 Nov 2018: 2011), ‘The computation of the spectra of highly. oscillatory Fredholm integral operators’, J.

26 Jul 2013: The slenderbody theory generates a system of Fredholm integral equa-tions of the first kind which are in general susceptible tooscillatory behavior or slow convergence in their numericalsolution, particularly when the

8 Jan 2008: Linear Analysis. T. W. Körner. January 8, 2008. Small print The syllabus for the course is defined by the Faculty Board Schedules(which are minimal for lecturing and maximal for examining). Several of the results arecalled Exercises. I will do

23 Aug 2023: This. isa. spec. ific. indiv. idual’s. copy. of. the. note. s.P. lease. do. not. copy. and/or. redis. trib. ute. Mathematical Tripos: Part III PM. Contents. 0 Perturbation Methods (16 Lectures) i. 0.1 Introduction. i. 1 Algebraic Equations 1. 1.1

SPECTRA OF GRAPH NEIGHBORHOODS AND SCATTERING. DANIEL GRIESER. Abstract. Let (Gε)ε>0 be a family of ’ε-thin’ Riemannian manifolds modeledon a finite metric graph G, for example, the ε-neighborhood of an embeddingof G in some Euclidean space

Dispersive hydrodynamics of soliton condensates forthe Korteweg-de Vries equation. T. Congy, G.A. El, G. Roberti, and A. Tovbis. Abstract. We consider large-scale dynamics of non-equilibrium dense soliton gas for theKorteweg-de Vries (KdV) equation

6 Dec 2020: σess(T) = {z C : T zI is not Fredholm}, ress(T) = sup{|z| : z σess(T)}.

21 Sep 2005: Evenmore ambitious goal is the analysis of highly oscillatory Fredholm equationsof the second kind.

23 Sep 2020: royalsocietypublishing.org/journal/rspa. ResearchCite this article: Colbrook MJ, Kisil AV. 2020 AMathieu function boundary spectral methodfor scattering by multiple variable poro-elasticplates, with applications to metamaterials andacoustics.

Soliton-mean field interaction in Korteweg-de Vriesdispersive hydrodynamics. Mark J. Ablowitz1, Justin T. Cole2, Gennady A. El3, Mark A. Hoefer1, andXu-dan Luo4. 1Department of Applied Mathematics, University of Colorado, Boulder2Department of

4 Aug 2009: The A-lines of an ultrasound imaging system can be mathematically modelled as a Fredholm inte-.

Soliton Gas: Theory, Numerics and Experiments. Pierre Suret,1, Stephane Randoux,1 Andrey Gelash,2 Dmitry Agafontsev,3, 4 Benjamin Doyon,5 and Gennady El4. 1Univ. Lille, CNRS, UMR 8523 - PhLAM - Physique des Lasers Atomes et Molécules, F-59000 Lille

26 Jul 2013: J. Fluid Mech. (2012), vol. 700, pp. 105–147. c Cambridge University Press 2012 105doi:10.1017/jfm.2012.101. Hydrodynamics of self-propulsion near aboundary: predictions and accuracy of. far-field approximationsSaverio E. Spagnolie1,2† and Eric

26 May 2010: A.1 Ultrasound image formation. The A-lines of an ultrasound imaging system can be mathematically modelled as a Fredholm in-.