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doi:10.1016/j.jcp.2004.11.039
www.itg.cam.ac.uk/people/heh/Paper187.pdf5 May 2006: and 4190, respectively. The corresponding values for ice were taken as 2.20 and 4190. ... Fig. 9. The heat loss factor against radius for the case k = 0.20 with1600 particles (40 40). -
The slumping of gravity currents
www.itg.cam.ac.uk/people/heh/Paper32.pdf30 May 2006: 0 20 40 60 80 100 120 140 160. t (9 FIGURE 2. ... 796 H. E. Huppert and J. E. Simpson. 0 10 20 30 40 50 60 70. -
PII: 0012-821X(82)90155-8
www.itg.cam.ac.uk/people/heh/Paper45.pdf27 Apr 2006: Petrol. 20 (1979) 487-554. 2 H,E. H u p p e r t and J.S. ... 100 (1980) 367-384. 20 E. Stolper and D. Walker, Melt density and the average. -
PDF/48/aa5873-06.pdf.url
https://people.ast.cam.ac.uk/~wyatt/lwbd06.pdf14 Dec 2006: 2004).These two stars are 10–20 Myr old (see Favata et al. ... 1 AU) while (sub)mm surveys probe cold dust (20 K)distant from the star (100’s AU). -
On gravity currents propagating at the base of a stratified ambient:…
www.itg.cam.ac.uk/people/heh/Paper184.pdf5 May 2006: . (2.20). Gravity currents propagating at the base of a stratified ambient 77. ... 2. 4. 6. 8. 10. 12. 14. 16. 18. 20. S = 0.7. -
Axisymmetric gravity currents in a porous medium
www.itg.cam.ac.uk/people/heh/Paper189.pdf5 May 2006: r (cm)0. 2. 4. 6. 8. 10. 20 30 40 50 6010. ... h/(Q/g′)1/2 = 9.2(1 – y). 0. 5. 10. 15. 20. 0.2 0.4 0.6 0.8 1.00. -
PII: 0012-821X(90)90126-I
www.itg.cam.ac.uk/people/heh/Paper98.pdf27 Apr 2006: b Institute of Theoretical Geophysics, University of Cambridge, 20 Silver Street, Cambridge CB3 9EW, U.K. " ... 100. 8O. 60. 40. 20. O " '. ". ' ". " ' -. 0 50 100 150 200. TIME (yrs) Fig. -
doi:10.1016/j.jcp.2005.12.002
www.itg.cam.ac.uk/people/grae/74.pdf12 Jun 2006: 17]), volume-averag-ing method (e.g. [18]), or by considerations of local thermodynamic balances [19,20]. ... 102 103 1.01 1.02 1.02 1.02104 1.41 1.69 1.67 1.70105 3.17 3.80 4.09 4.195 105 5.24 6.20 -
mnr_7037.tex
https://people.ast.cam.ac.uk/~wyatt/gw03.pdf19 Apr 2006: and Spangler et al. (2000) are also included here – ISO observed 70per cent of the single A stars but only 20 per cent of single G starswithin 25 pc. ... If the r 3 line in Fig. 2 is extrapolatedfrom 20 to 25 pc, the detections should increase to 20 -
Collapses of two-dimensional granular columns Gert Lube,1 Herbert E.…
www.itg.cam.ac.uk/people/heh/Paper190.pdf5 May 2006: Unknown to the present authors, a similarstudy was undertaken by a French group 20. ... S. J. Sparks, and M. A. Hallworth,. J. Fluid Mech. 508, 175 2004.20 E. -
Brains and Persons | Faraday
https://www.faraday.cam.ac.uk/resources/multimedia/brains-and-persons/18 Jul 2006: 480x360. 855.54 MB. WebM. 480x360. 443.84 MB. 480x360. 257.20 MB. 320x240. -
AccFinalPaper.dvi
www.statslab.cam.ac.uk/~rjs57/AccFinalPaper.pdf3 Feb 2006: tion to λ1,. , λM1, though since one individual died aged 20.5 years in auricular. ... surface stage 2, we constrained a to lie between 0 and 20 years. -
85230
www.itg.cam.ac.uk/people/heh/Paper146.pdf27 Apr 2006: 46, p. 11–20. Hutter, K., Koch, T., Plüss, C., and Savage, S. ... 362–368. Manuscript received February 20, 1998Revised manuscript received June 1, 1998Manuscript accepted June 17, 1998. -
Flow focusing instability in a solidifying mushy layer
www.itg.cam.ac.uk/people/grae/25.pdf1 Jun 2006: 0. P. Chiareli and M. G. Worster. 0 5 10 15 20 4 &. FIGURE 2. ( a ) Dispersion relation i, us. 8 for equation! ... 0 - / 0 /. / - 0 20 - / 4 - -. I I I I. 303. 60. -40. 20. 0. 120. 80. % -
Nonlinear double-diffusive convection
www.itg.cam.ac.uk/people/heh/Paper25.pdf30 May 2006: 3 5 0.40 0.45. 2.h 2.1P. I I I I I I 0.19 0.20 0.21. -
Some remarks on the initiation of inertial Taylor columns
www.itg.cam.ac.uk/people/heh/Paper19.pdf30 May 2006: 3.20) /Om. where the kernel. and &t) is the zeroth-order Hankel transform of h ( r ) , given by. ... 20, 429-448. Ocean. I n s t. G.F.D. Notes, no. 2, pp. -
PRL 95, 176102 (2005) P H Y S I ...
www.itg.cam.ac.uk/people/grae/65.pdf26 Apr 2006: D3H000. 1. D3. 0 0; (20)which we integrate with H001 D001 0, D00 , and D01 0 to obtain. -
THE INVARIANTS OF A GENUS ONE CURVE TOM FISHER ...
https://www.dpmms.cam.ac.uk/~taf1000/papers/g1inv.pdf9 Oct 2006: For details in thecase n = 3 we refer to [13, Exercise 13.20] or [25, 4.4]. ... Then byProposition 5.19 and Lemma 5.20 there is an isomorphism γ : Cφ = Cφ′with γωφ′ = ωφ. -
Natural Convection, Solute Trapping, and Channel Formation during…
www.itg.cam.ac.uk/people/grae/33.pdf26 Apr 2006: In a series of 13experiments,2 solutions of different initial concentrations of NaCl(ranging from 1 to 14 wt %) were placed in a rectangular cell20 20 28 cm, the upper boundary -
Convection and particle entrainment driven by differential…
www.itg.cam.ac.uk/people/heh/Paper99.pdf30 May 2006: t would have the same settling velocity in water a t 20 "C. ... 0655. R 0.01 0.14 0.22 0.28 0.44 0.63 0.84. 0 5 10 15 20.
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