Search

Search Funnelback University

Search powered by Funnelback
10 results 20 results 50 results
Relevance Date (Newest first) Date (Oldest first) Title (A-Z) Title (Z-A) Distance URL (A-Z) URL (Z-A) Shuffle
11 - 20 of 20 search results for TALK:PC53 20 |u:www.damtp.cam.ac.uk where 0 match all words and 20 match some words.

  1. Results that match 1 of 2 words

  2. 5 May 2008 National Transport Information Incubator (NaTII) Enabling…

    www.damtp.cam.ac.uk/user/pvl/natii_publication.pdf
    13 Jun 2008: It focuses on:.  visual and simple.  the fact that the first 20% of effort gets 80% of the result.

  3. On Dynamics and Transport Near the Polar Mesopause in Summer

    www.damtp.cam.ac.uk/user/mem/mcintyre-mix-efficiency-jgr89.pdf
    23 Sep 2008: JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 94, NO. D12, PAGES 14,617-14,628, OCTOBER 20, 1989. ... r {-«Z3m a(sin Zm - Zm cos Zm)} (20). lfOZm AA = • -(z 2 - a 2 sin 2 z)dz - 3 -- •Zm q- «a2(zm- sinzm coszm)} (21).

  4. B9Lb.dvi

    www.damtp.cam.ac.uk/user/examples/B9Lb.pdf
    30 Sep 2008: ψ(x, t) = χ(x) exp. (. iEt. ). (20). Substituting for (20) for ψ in the Schrödinger equation yields the time-independent. ... States of the special form (20) are known as stationary states.

  5. Mathematical Tripos: IA Vector Calculus Contents 0 Introduction i ...

    www.damtp.cam.ac.uk/user/sjc1/teaching/VC_2000.pdf
    17 Jan 2008: whenever this limit exists. Remarks. • It follows from (1.20) and the definition of a partial deriva-tive (1.14) that. ... To derive (1.52) start from the definition of a directional derivative (1.20), and use the definition of.

  6. Preprint typeset in JHEP style - PAPER VERSION June ...

    www.damtp.cam.ac.uk/user/tong/tasi/tasi.pdf
    24 Apr 2008: 1.4 The ADHM Construction 20. 1.4.1 The Metric on the Higgs Branch 23. ... 20 –. of the D(p 4)-brane [3, 5]. They are the same object!

  7. ��������� � ���� ������ ����� ����������������� �! "��#$�…

    www.damtp.cam.ac.uk/user/ngb23/publications/potential7.pdf
    1 Feb 2008: 0 10 20 30 40 50 600. 5. 10. 15. 20. ... 3è1V6ñEG;=1"J /. i>31Vð@6:v3EF<@> <Cç35è1ENêïé-DF;1þ:C>-A 17>1V6ð"õÂ651V;éDN35;zEF> :@>. 5. 0 10 20 30 400.

  8. D23Ld.dvi

    www.damtp.cam.ac.uk/user/examples/D23Ld.pdf
    5 Dec 2008: 20. Cop. yrig. ht. 200. 8 U. nive. rsity. of C.

  9. Adv. Geosci., 15, 47–56, 2008www.adv-geosci.net/15/47/2008/©…

    www.damtp.cam.ac.uk/user/mem/mci-jet-hyperb-ADGEO-08.pdf
    1 Jul 2008: ρ0. z. (ρ0f. 20. N2. ψ′. z. )= q′ , (15).

  10. Multiple Jets as PV Staircases: The Phillips Effect and ...

    www.damtp.cam.ac.uk/user/mem/dritschel-mci08.pdf
    1 Apr 2008: 7b) and, with H0 f 20 L. 2D /g, the undisturbed layer depth,.

  11. A Theoretical Framework forBackward Error Analysis on Manifolds…

    www.damtp.cam.ac.uk/user/na/NA_papers/NA2008_02.pdf
    27 Jan 2008: 20. for sufficiently small t. We will prove this. Let (U,ϕ) be a chart containing p then, in thesecoordinates, τ will have the form.

Refine your results

clear all

Date

Search history

Recently clicked results

Recently clicked results

Your click history is empty.

Recent searches

Recent searches

Your search history is empty.