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GRAVITY WAVE GENERATION BY VORTICAL FLOWS IN A ROTATING ...
www.damtp.cam.ac.uk/user/mem/papers/SSREPLY/rupert-ford-thesis93.pdf19 Oct 2013: compared with typical inverse time scales for the flo". A succession of balance inversion op-. ... The study of Lorenz 0. Krishnamurthy (op. cit.) was not confined to the limited regime where all trajectories approaCl. -
SHA.dvi
www.damtp.cam.ac.uk/user/na/people/Alexei/papers/dmrus.pdf1 Sep 2011: 0; h! 0;W TO WREMQ KAK DLQ p > 2 kD1hkLp(V ) = Op(1)h12=pj lnhj! ... 13:9)I WYPOLNENY OCENKI kf1kWmp (I4h) = Op(1); p 2 [1; 2);k(f1)kL1(Vh) = OH(j lnhj)! -
spn0.dvi
www.damtp.cam.ac.uk/user/na/people/Alexei/papers/spn0.pdf1 Sep 2011: 3. Acknowledgements. I am grateful to Prof. W. Dahmen for giving me the op-portunity to work at the RWTH Aachen, and for his constant inspiring encouragementof my studies. ... i j is js s, |i| :=. s. is. The following lemmas will be used frequently (see -
Natural Sciences Tripos, Part IB Michaelmas Term 2008 Mathematical ...
www.damtp.cam.ac.uk/user/gio10/nst_notes.pdf3 Oct 2008: ẑ). The position vector of a point P is. OP = r = exx eyy ezz =. 3. i=1. eixi. 1.2.2 Properties of the Cartesian unit vectors. The unit vectors form -
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www.damtp.cam.ac.uk/user/ngb23/publications/potential7.pdf1 Feb 2008: Aé13<K3è-1 ->EN31ZEF>"3517ð"65:C3EF<@>kA<@ê|:CEF>. S 0 ù ûèé-;Vü35è1zî@1VDN<ì4EN3õþ<Cç3è1î"<@6317òEG;><@3K35è19;éê
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