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D22Lb.dvi
www.damtp.cam.ac.uk/user/examples/D22Lb.pdf25 Jan 2007: Recently an outstanding new textbook book came out which I strongly rec-ommend for the physical side of GR. ... This allows us to pass to a new(non-inertial) coordinate system. x̃ = x b(t), (17). -
Operator theory and C∗-algebras in infinitedimensional numerical…
www.damtp.cam.ac.uk/user/na/NA_papers/NA2007_04.pdf13 Apr 2007: HansenUniversity of Cambridge. Abstract. We present several new techniques for approximating spectra of linear operators (notnecessarily bounded) on an infinite dimensional, separable Hilbert space. ... new developments in the self-adjoint case[Dav00], -
IOP PUBLISHING CLASSICAL AND QUANTUM GRAVITY Class. Quantum Grav. ...
www.damtp.cam.ac.uk/user/md327/dunajski_hartnol.pdf17 Apr 2007: A crucial new aspect ofthe asymptotically locally Euclidean and asymptotically locally flat Israel–Wilson–Perjéssolutions is that when. -
220_2007_208_Article.dvi
www.damtp.cam.ac.uk/user/md327/Dunajski_West.pdf27 Jul 2007: In the proof we will oftenuse the following shorthand for coordinate transformations: t F(t, x, y, z) meansdefine a new coordinate t̃ = F(t, x, y, z) and then relabel ... This avoids havingto introduce new symbols for new coordinates. We will denote -
Do Rossby-wave critical layers absorb, reflect, or over-reflect?
www.damtp.cam.ac.uk/user/mem/killworth-mcintyre-jfm85.pdf5 Dec 2007: The mathematical tool on which the general proof depends is a finite-amplitude conservation theorem for time-dependent disturbances to parallel shear flows, which appears to be new and which generalizes
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