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8 Jul 2024: 20. Worster, M.G. 1993. Book review of "Mathematical Modeling of Melting and Freezing Processes" by V.

23 Nov 2005: 20 October. Stephen Morris. (Toronto and DAMTP). Dirty water, chemical plumes and cracking mud.

11 Feb 2003: Liora Malki. (ITG). TBA. 20 February. Tom Hulme. (Bullard). Seismic scattering from small-scale heterogeneities.

5 Oct 2009: 20 October. Sue Liu. (DAMTP). Transport and dehydration in the tropical tropopause layer.

8 Oct 2008: 13 November. Peter Liss. (UEA). Air-sea exchange of trace gases. 20 November.

9 Oct 2007: 20 November. No seminar. 27 November. Jessica Irving. (ITG). Inner core anisotropy.

29 Jan 2003: 20 February. Andy Woods. (BPI). Models of flows in oil reservoirs.

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

9 Mar 2004: In addition, during such eruptions magma heating orcooling may also occur9,19,20, especially after input of hot basalticmagma at the base of the chamber18. ... eruptions. Earth Planet. Sci. Lett. 114, 505–516 (1993). 20. Floch, A. &

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

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.

11 Apr 2013: 20. 40. 60. 80. 100. 120. 1 2 3 4 5 6 7. ... E. Huppert, J. A. Neufeld and C. Strandkvist. 0 20 40 60 80 100.

19 Jul 2010: All the experiments were carried out using a Perspex container, 50 x 20 x 40 cm high. ... t Ice Na2C03.10H20. -10' I I I I I I 0 5 10 15 20 25 30.

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.

18 Jan 2007: Peppin, P. Aussillous, H. E. Huppert and M. G. Worster. 5 10 15 20 250. ... J. Cryst. Growth 20, 121–124. Chen, C. F. 1991 Experimental study of convection in a mushy layer during directional solidification.J.

25 Nov 2011: T̄. (νB2H 3/2W 3/2. gV 20. )1= 4. 9 sin θ(a1/2 a1/2 tan1/3 θ )3,. ... V̄ = V0(t/T̄ )1/2, (5)using Eqs. (2)–(4). Note that T̄ V 20 from Eq.

8 Jun 2012: 10. 12. y (mm). z (m. m). t=2mint=10mint=30mint=40minbase. 60 40 20 0 20 40 600. ... Academic Press, New York (1977). 20. Rajchenbach, J.: Dense, rapid flows of inelastic grains under grav-ity.

16 Jul 2010: base o f a container 10.6 x 20 x 30 cm high. ... A ft er some 20 to 30 minutes f r o m the beginning o f the experiment the release o f light fluid is greatly accelerated and penetrates through 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.

9 Feb 2004: Runs prefixed by the letter A were condin the 1m long tank (w5 15 cm!: those prefixed by the letter B in the 2 m long tank (w5 20 cm! ... a rapid initial decrease between 0 and 20 cm, then levels out as a shoubefore steepening sharply at approximately 75

14 Sep 2009: Style1 and M. Grae Worster1. Received 22 January 2009; revised 20 April 2009; accepted 6 May 2009; published 10 June 2009.

26 Sep 2011: 5) Huppert, H. E.; Manins, P. C. Deep-sea Res. 1973, 20, 315-23. ... 7 = 0.287. The cross-terms are 20 times less than the smallest main term.

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.

26 Mar 2023: In the case α = π/4, for example,the domain size is given by a = 5, b = 20 and c = 15. ... 14. Cambridge, UK: CambridgeUniversity Press. 20. Hewitt DR, Balmforth NJ. 2013 Thixotropic gravity currents.

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

25 Nov 2011: A cutoff of either 20% or 40% of the total concentration was used to determine the position of the front. ... A cutoff of either 20% or 40% was used to determine the front position.

18 May 2017: radius R 20 mm, half thickness W 0.04 mm, and atypical time scale halfway through an experiment t 100 s,the effective Reynolds number in the crack is Reeff ρurW2μ1R1

13 Apr 2011: H 20 m,motivated by the Sleipner site in the North sea [Bickle et al.,2007]. ... FCO2 DDCO2. HSh DCO2. kgD. 4=5 DH. 1=5. ’ 20 kg m2 yr1.

15 Jul 2010: 2a). Angles of 90” (vertical), 70”, 45 O and 20 O were all utilized. ... Fig. 8. Compositional profiles of solutions for slopes of 20 (o), 4S” (0).

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.

24 Aug 2011: 3.3mm per year, remarkably uniformly for at least the last 20 years. ... so to influence the result in 10, 20, … years’ time we need to act now.

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.

22 Jan 2007: 1 mm. 20 wt% montmorillonite. 1 mm. (a) (b) (c). (d) (e) ( f ). Figure 1. Colloidal suspensions frozen by cooling from below. The system is open at the top to asupply ... where CiZCN/ks. Equation (2.20) can be integrated from zZ0 to z ZN usingequation

20 Nov 2014: Jacobel, R. W., A. Robinson, and R. A. Bindschadler (1994), Studies ofthe grounding-line location on Ice Streams D and E, Antarctica, Ann.Glaciol., 20(1), 39–42.

26 Mar 2023: n 20. 22 a. t 22:. 35:0. 9, s. ubje. ct to. ... To begin, by equating the predictions for the ratio of viscous tobuoyancy forces (A1 = A2) given by (2.18) and (2.20), we obtain, on simplification,.

17 Jan 2019: Our theoretical understanding of thesolidification of binary alloys is well-developed [19,20]. ... a 160 10% 9 mA 3.67 10% 20 Jl 0.225 e.

23 Dec 2021: For an inverse cone, τ ′ is given by. τ ′=20.4p1[10.049p0(p2)], (2.8). ... 5.1) becomesHT γ. 5/20 (H. 3Hx)x =0. (A 9). Dow. nloa.

26 Mar 2023: vN /(4β sin α tan α) 4 tan αs1/20 [(s s0)3/2 s3/20 ]/3 = A.

9 Mar 2004: 10. 1. 0.1102 103 104 105. 20 h10 h1 h. Time (s). ... 20. 105. 119. 105. 82. 55. 28. 6.3. 2.5. t (h).

14 May 2008: S. L. Peppin, H. E. Huppert and M. G. Worster. 0 5 10 15 20. ... JOM-J. Min. Met. Mat. Soc. 49, 18–20. Huppert, H. E. 1990 The fluid mechanics of solidification.

2 Apr 2007: The experiments werecarried out using cylinders and rectangular tanks 30 to 60 cm tall, and cover aspectratios between 0.5 and 20, where the aspect ratio is defined as the ratio ... 6. 4. 2. 0 5 10 15 20. Hei. ght (. cm). Horizontal distance (cm). XY. XY.

24 Sep 2014: Experienced volcanologists say there is a 20% chance of a huge eruption on. ... people and injuring a further 70. The immediate response was to curtail train speeds, in some places to as low as 20 mph from 125 mph.

9 Oct 2015: Peppin). The width of the view is approximately 20 cm. (Online version in colour.). ... J. Geophys. Res. Oceans 118, 2279–2294. (doi:10.1002/jgrc.20171). 20. Griewank PJ, Notz D.

9 Feb 2004: η = 4ρpQϕ0(R6 3R2 2)/(3πr2), (2.20). which is also plotted in Figure 1. ... u = u0 = (kgQ0/βl0)1/2 (l = l0 = kgQ0/βu. 20), (3.15).

8 May 2007: h. t+. 8g sin β. 15νh2. h. z= 0. (2.20). The effect of confining boundaries on viscous gravity currents 499. ... 10. 20(a) (b). t/(v/ga). 103 104 105. t/(v/ga). z N /. (V/a. )1/2. 10. 100. z N /. (V4 s. in3 β.

26 Mar 2023: Thisprediction might be different if we considered a model using the adaptation of Darcy’s Law posedby Forchheimer [19], or that posed by Brinkman [20] (specifically designed for transitions fromnon-Darcy ... Z. Ver. Deutsch. Ing. 45, 1782–1788.20.

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.

9 Mar 2004: 10. 1. 0.1102 103 104 105. 20 h10 h1 h. Time (s). ... 20. 105. 119. 105. 82. 55. 28. 6.3. 2.5. t (h).