Search
Search Funnelback University
- Refined by:
- Date: 2011
1 -
10 of
22
search results for b&b |u:www.damtp.cam.ac.uk
Fully-matching results
-
www.damtp.cam.ac.uk/user/gold/pdfs/teaching/double_layer_prl.pdf
www.damtp.cam.ac.uk/user/gold/pdfs/teaching/double_layer_prl.pdf10 Apr 2011: -
nis2.dvi
www.damtp.cam.ac.uk/user/na/people/Alexei/papers/nis2.pdf1 Sep 2011: The general problem is to nd the complete collection G = f(A;B)g of sharpconstants in (1.1) which are dened as(1.2) A A0 := inf(;)2 ; B := ... Bojanov, ed.), SCT Publishing, 1994, pp. 192{204.5. S. B. Stechkin, Best approximation of linear operators, -
Multicellularity and the functional interdependenceof motility and…
www.damtp.cam.ac.uk/user/gold/pdfs/multicellular.pdf10 Apr 2011: 1. Enquist, B. J. & Niklas, K. J. (2001) Nature 410, 655– 660.2. ... Schulz, H. N. & Jørgensen, B. B. (2001) Annu. Rev. Microbiol. -
Concentration Dependence of the Collective Dynamics of Swimming…
www.damtp.cam.ac.uk/user/gold/pdfs/sokolov_prl.pdf10 Apr 2011: b). Vector fields for velocity V (c) andorientation (d) for the configuration shown in image (b). ... KrZdr0. Z 20d hVr0 Vr r0ihVr0i2:. The correlation length was extracted from Kr by a fit toan exponential, Kr expx=L B, B const. -
INSTITUTE OF PHYSICS PUBLISHING NONLINEARITY Nonlinearity 18 (2005)…
www.damtp.cam.ac.uk/user/gold/pdfs/spin.pdf10 Apr 2011: F = qE qc. pm. B (B)m. (6)We now introduce into (4) and (5) the following representation for f1,. ... iη. t= 1. 2m. (iη e. cA. )2 e eη. 2mcσ̂ B, (38). -
Boundary layer model for vortex fingers in type-II superconductors ...
www.damtp.cam.ac.uk/user/gold/pdfs/vortex_fingers.pdf10 Apr 2011: time in units of th = Cd / h, currents inunits of jc0, and fields as b = B / B1, B1 = 4Jc0Lh / c. ... Blatter, M. V. Feigel’man, V. B. Geshkenbein, A. I. Larkin,and V. -
einstein_brownian
www.damtp.cam.ac.uk/user/gold/pdfs/teaching/einstein_brownian05.pdf10 Apr 2011: holds. B B 'But from this and the last equation obtained itfollows that. -
��������� ��� � ����������� ������� �"!$#%'&�( )…
www.damtp.cam.ac.uk/user/gold/pdfs/spiral.pdf10 Apr 2011: $&' &( ) ,-/.01324/56378/9:;%<=?>A@B CEDFHGJIKLMNPORQTSUSWVYXZ[]%_Aa/bcAdefAggAhiAjkl/mnAop/qrs%tuAuWvw x%yzY{|}JP W WW P ¡¢£¤ ¥«ªHµº º» ¿ÀRÁÂÃÃÅÄÆÇÄ ÈÉËÊÌ?ÍÎ ÏÑÐÅÒÒÓ Ô. ... $#&%' (),-. /0123456798 :<; =?> @&ACB?D EEF -
Mathematical Tripos Part III 2007–08Fundamentals of Atmosphere–Ocean…
www.damtp.cam.ac.uk/user/mem/III-NOTES/mcintyre-fund-atm-oc-dynamics-exs-3.pdf15 Jul 2011: 12 f ). Allow fora sloping bottom boundary z = b(x, y), taking care to distinguish between the layer depth h andthe free-surface elevation ζ(x, y, t). ... b = b(y) =. {. ǫa, y > aǫy, |y| < a. -
AJP Journal
www.damtp.cam.ac.uk/user/gold/pdfs/teaching/van_der_waals.pdf10 Apr 2011: n. -. ir. e. V R!52 23 a E. 2 1 b M2! ... Laloe, Quantum MechanicsWiley,. New York, 1977!, Chap. XI.12See, e.g., B. R.
Search history
Recently clicked results
Recently clicked results
Your click history is empty.
Recent searches
Recent searches
Your search history is empty.