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26 Apr 2006: VOLUME 87, NUMBER 8 P H Y S I C A L R E V I E W L E T T E R S 20 AUGUST 2001. ... Silver Street, Cambridge CB3 9EW, United Kingdom(Received 20 March 2001; published 7 August 2001).

27 Apr 2006: N. W i l s o n a. a Department of Geology, Wills Memorial Building, Bristol University, Bristol BS8 1RJ (U.K.) b Institute of Theoretical Geophysics, 20 Silver Street, University

27 Apr 2006: Herbert E. Huppert and M. Grae Worster 1. Institute of Theoretical Geophysics,University of Cambridge, 20 Silver Street, Cambridge CB3 9EW, UK. ... First, we wished to apply an concentration,the z. 1 werechosentobe(10, 20, 30)additional test to the

26 Apr 2006: D3H000. 1. D3. 0 0; (20)which we integrate with H001 D001 0, D00 , and D01 0 to obtain.

27 Apr 2006: Herbert E. Huppert and M. Grae Worster 1. Institute of Theoretical Geophysics,University of Cambridge, 20 Silver Street, Cambridge CB3 9EW, UK. ... First, we wished to apply an concentration,the z. 1 werechosentobe(10, 20, 30)additional test to the

30 May 2006: a 3 ) ( 2 ) - (0 < 01 < 1) (2.20 c). ... 2 1 ) ; part of (2.20); and part of (2.17) [and none of (2.16)].

28 Jul 2006: 5. 50% most cited (/yr) 21( 0.6) 21( 0.8) 20( 1.3) 6( 1.2). ... 1970-1975 1975-1980 1980-1985 1985-1990 1990-1995 1995-2000 2000-2005 2005-2010. 0. 10. 20.

26 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

27 Apr 2006: y = yj[1 — 0.015(20— T)], (2.2). ___________ where T is the temperatureof the liquid injant now degreesCelcius,andL79X2C2. ... 1.0 cal cm3 oCl medium,and this bound is attainedfor the spe-20 C cial caseof parallel rods or lamallae when the.

27 Apr 2006: wt% H2SO4. 0. 1,000. 2,000. 3,000. Dep. th (m. ). –35 –30 –25 –20 –15 –10 –5Temperature (C). ... 600 m above the base (20% of the 3,000-m ice thickness) and an accumulation rate of.

27 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.

1 Jun 2006: A. V. FURSIKOV. Kluwer, 1988. 576 pp. $149 or $90. 20, v ) = exp ( i ( v , u)) drut(u).

27 Apr 2006: 0.10. 0.20, 0.30, 0.50 and 1.0 wt% CuSO4, The sameinitially contaminatedwith 0. ... z 5 39S S. 20 S • •38.5 -. 0 I I -0 100 200 300 400 500.

5 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.

1 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. %

26 Apr 2006: 0.5. -20. -10. -5. -0.5. 1. 3. 5. 7. 5 cm. ... 5 10 15 20 25 30 35 40. 0.2. 0.4. 0.6.

26 Apr 2006: Curvature effects can be neglected whenR4Rc and analytical expressions for Vc arereadily derived [20]. ... Cambridge, 1999, p. 339. [20] A.W. Rempel, M.G. Worster, J. Crystal Growth 205.

30 May 2006: I found only one obvious error. I n Section 6.6 the angle q5 is used in the text, while it is depicted as 8 in figure 6.20 ; and qi

28 Apr 2006: up. The resistance between thewires is almost negligible, and hence the functional form ofthe conductivity at a fixed temperature 20 is. ... 20 0:0015T: ð7ÞHere T is the temperature deficit below 20 C, S is in ppt.

30 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.

27 Apr 2006: 2.20) It is of interest to know at what value of k the. ... 1992) 487.8. References [20] V.V. Vas’kin, Izv. Akad. Nauk SSSR, Metally 1)1986) 83.

1 Jun 2006: 2= 307 J 337 J 20.0 "C. A 0.056 -. TABLE 1. ... 10. 5 -. 35 1. -. - h. E 0. 0 10 20 30 40 50.

26 Apr 2006: Cambridge CB3 9EW, UK. Received 27 March 1999; accepted 20 August 1999Communicated by D.T.J. ... h"hi#(h. =!h. i) erf (X1@2g/2), (20). where erf(x) is the error function given by.

5 May 2006: 10. 5. 0 5 10 15 20. Figure 1. A shadowgraph image of the developing cells after 7 min. ... 1 48.2 20.3 20.3 7 1.47 1.1 4250 1.1 0.73 48.2 20 20.3 40 0.85 2.6 1810 2.7

17 May 2006: 358 D. Vella and H. E. Huppert. –2 –1 0 1 20.

27 Apr 2006: 2.20) It is of interest to know at what value of k the. ... 1992) 487.8. References [20] V.V. Vas’kin, Izv. Akad. Nauk SSSR, Metally 1)1986) 83.

30 May 2006: BLANCH, G. 1964 Mathieu Functions, chapter 20 in Handbook of Mathematical Functions (edited by M.

11 Oct 2006: t. θ. 5 10 15 20 25 3010–4. 10–3. 10–2. 10–1. ... 374 M. Ungarish and H. E. Huppert. t0 4 8 12 16 20 24.

5 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.

30 May 2006: Huppert and A. W. Woods. 0 20 40 60 80 100. ... Gravity-driven flows in porous layers 61. 100. 80. 20. FIGURE 4.

30 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.

26 Apr 2006: cooled and solidified from above. The apparatus consisted of a Perspex tank, withwalls 11 mm thick, of dimensions 20 20 37.6 cm with a brass lid as depicted infigure 1. ... E. Huppert. (a). 12. 8. 4. h (cm). (b). T B = – 20 C.

27 Apr 2006: 1998] of 0.20. Thecalculated mean area covered by melt ponds on first-yearice was 0.41. ... Remote Sens., 20(10), 2069–2090. Derksen, C. P., J. M. Piwowar, and E.

27 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.

26 Apr 2006: 0.4; (d) latex withG104 K m1 [20], slope! 1.0; (e) latex with G4]104 K m1 [21], slope! ... dt. dd0. dd0, (20). where d0(t"0) is the initial "lm thickness at h"0.

30 May 2006: Physics, University of Cambridge, 20 Silver Street, Cambridge CB3 9EW, UK 2Department of Geology, University of Bristol, Bristol BS8 lRJ, UK. ... y = 0 ( t = t,), (3.20). where t, is the time for the initial current to attain the slumping distance x,.

1 Jun 2006: Huppert. To cooler. - I 20 cm l o - 10 cm I 1 Scale. ... A. - 0. -10. T ("C). -20. -30. 100. Source. E D B, n C D.

17 May 2006: 20. The curves for solutions S3 and S4 are identical to within the. ... Liquid rope coiling 291. 10. 20. 30. 40. 50. 7 8 9 10.

26 Apr 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).

30 May 2006: Substituting (2.19) into (2.20), we obtain. to which must be added the global continuity equation. ... 5 = (fg1Q3/V)-Brt-(3i1)/8 and. h(r> t , = @“(3&V/g’)a $([/EN),. (2.20).

11 Oct 2006: Statistical studies of the globaldatabase suggest that for volcanism more than 2000 years ago, only 20% of largemagnitude explosive eruptions have been recognized. ... The historiccatalogue, and in particular the 20 year period of analysis in this study,

1 Jun 2006: 50. 40. 30. 20. 10. R m. 0. I I I I I I? ... E = 0.0125. 5 10 15 20 25 30 a. a FIQLJRE 8.

26 Apr 2006: for heat and salt,respectively.[20] The ratio of exchange coefficients ah/as depends on. ... Asshown in Figure 6, the calculated ablation rates vary byabout 20% for a reasonable range of these coefficients.

5 May 2006: 10 7 Tb (C) 20 20 20 20 20 20. ... 0.62.7. 5.7. 0 2 4 6 8–20. –15. –10. –5. 0.

30 May 2006: Turning now to the evaluation of cl (g,?), we substitute (2.20) into (2.16)). ... u and v and also the fact that V2S, = 0 [(2.20) and (2.25)].

5 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).

1 Jun 2006: C. Kerr. L. 0.25. 5 0.20 F,. 3. e 5 0.10 8. ... k, kt 9,. P. T, 20. 100.8 10 D 2.5 x lo-' 0.93 x lo-' Y.

12 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

1 Jun 2006: K. 4. Experimental apparatus and procedure The experiments were performed in a glass tank 20 cm wide filled to a depth of. ... 20 cm with a mixture of glycerine (30 w t Yo) and water (see figure 4 ). The length of the tank was varied so that results were

30 May 2006: be explicit) in a rectangular Perspex tank 40 x 20 x 30 cm high. ... Each ice block was approxi- mately 3 x 15 x 20 cm high.