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9 Mar 2004: flow. Pyroclastic flows can be up toseveral thousands of cubic kilometres in volume, propagating for tens of kilometresfrom the vent of a volcano at speeds over 200 m s1 (Sparks et ... ume. Vmax30. 0t. (b). Vmax. 200 400 600 800 1000. 25.

26 Apr 2006: thickness around day 200 is due toflushing of surface melt water through an artificial bore holeand the creation of a false bottom.

22 Mar 2007: tters 255 (2007) 164–176www.elsevier.com/locate/epsl. Earth and Planetary Science Le. Modelling carbon dioxide accumulation at Sleipner: Implicationsfor underground carbon storage. Mike Bickle a,⁎, Andy Chadwick b, Herbert E. Huppert c, Mark

27 Apr 2006: Fluid Mech. 33 (1968) 183-200. 16 H.E. H u p p e r t and P.F.

12 Jun 2006: We then adapt our code to the configurationof Worster [1]. Since analytical results are obtained in a semi-infinite domain, we impose a very large aspectratio w/h = 200 and choose

24 Apr 2014: year1 (megatonnes CO2 injected per year) since 1996 into the Utsira sandstone, a 200–300-m-thick, highly porous, and permeable reservoir. ... 1,200. 1,300. 1,400. TWTT. (ms). W E. TUTU. BUBU. IHIH. TU.

5 May 2006: Perspex, 1.1 cm thick, with internal lengths and depths of 50 cm 30 cm, 200 cm 22.3 cm and 232.5 cm 40 cm.

15 Sep 2006: 400. 300. 200. a). BS. 100 2O0 300. TIME (yre). S! ... 100. 400. b). 100 200. TIME (yre). 300 4OO. FIG 5 Variations of (a) temperature, and (b) thickness of the silicic magma layer with time for a 500 m thick sillemplaced

27 Apr 2006: Glaciol., 33, 194–200. Eicken, H., H. R. , .

9 Mar 2004: 1125WETTLAUFER ET AL.: SOLIDIFICATION OF LEADS. profile was taken after the buoy had reached the oceanic tem-perature, and each subsequent profile is separated by 200 min.A quantitative analysis of ... The initial profile was taken after the buoy had

30 Jun 2010: 442 H. E. Huppert and P. P. Linden. 220. 200. 160 l.

9 Mar 2004: The simulations discussed here were obtained for a channel of length xw = 4,the typical grid had 160 horizontal and 200 stretched vertical intervals, and thetypical time step was 2 103.

18 Sep 2006: In t h e case o f olivine, the best available estimate of L is 200 cal g m - 1 (Bottinga a n d Richet 1978), a n d ... 3. 100. o. z 200. I 0 I 0 0 I 0 0 0.

30 May 2006: 1. oo 1.712 1.26 1.42 1.10 1.24. 13.61 1.200 0.79 1.06 1.

21 Nov 2014: J. Fluid Mech. (2014), vol. 757, pp. 330–353. c Cambridge University Press 2014doi:10.1017/jfm.2014.469. 330. Fluid migration between confined aquifers. Samuel S. Pegler1,†, Herbert E. Huppert1,2,3 and Jerome A. Neufeld1,4. 1Institute of

9 Mar 2004: 25. 0 50 100 150 200 250. 50. 75. 100. 125.

18 May 2017: J. Fluid Mech. (2016), vol. 791, pp. 329–357. c Cambridge University Press 2016doi:10.1017/jfm.2015.733. 329. Stratified gravity currents in porous media. Samuel S. Pegler1,2,†, Herbert E. Huppert1,3,4 and Jerome A. Neufeld1,5,6. 1Institute of

9 Feb 2004: Quantitative modelling ofgranular suspension flows. By Herbert E. Huppert. Institute of Theoretical Geophysics, Department of AppliedMathematics and Theoretical Physics, University of Cambridge,. Silver Street, Cambridge CB3 9EW, UK. A broad review

17 May 2006: Liquid rope coiling 289. 0.6. 0.8. 1.0. 0.8. 1.0. 100 200 500 1000 2000 5000.

27 Apr 2006: that. a. b. µm0 100 200. Figure 1 The hydraulic system of polycrystalline ice. ... Separation (m). 2,000. 2,200. 2,400. 2,600. 2,800. 3,000. Dep. th (m. )

18 Jul 2014: J. Fluid Mech. (2014), vol. 745, pp. 592–620. c Cambridge University Press 2014doi:10.1017/jfm.2014.76. 592. Fluid injection into a confined porous layer. Samuel S. Pegler1,†, Herbert E. Huppert1,2,3 and Jerome A. Neufeld1,4. 1Institute of

18 Nov 2009: of storage for experiment 1 (), 2 (), 3 (), 4 () and 5 (). The horizontal dashedline indicates a storage efficiency of 50 % which was reached in approximately 20 T 200 s.

10 Jun 2004: J. Fluid Mech. (2004), vol. 508, pp. 175–199. c 2004 Cambridge University PressDOI: 10.1017/S0022112004009036 Printed in the United Kingdom. 175. Axisymmetric collapses of granular columns. By GERT LUBE1, HERBERT E. HUPPERT2,R. STEPHEN J. SPARKS1

30 May 2006: Y f 5 200 -. 6 a. 250 -. 300 -. Salinity ( % o ). I I I I I I I I 34.2 34.3 3 4 4 34.5 34.6 34.7 ... 200. n E. 300. 350. I I 0.1 OC. FIGURE 8.

9 Mar 2004: 200 points and with a time stepof 5 103.

18 May 2017: 0.25. 0.300 100 200 300 400 500 600. Reduced gravity with time offset.

14 Sep 2009: 0 50 100 150 200 2500. 0.5. 1. 1.5. 2. Time, minutes.

5 May 2006: Details of our finite-difference numericalcode are presented the Appendix. We used a mesh of 320 horizontal and 200 verticalintervals.

11 Apr 2013: Gravity and flow focusing in two-layered porous media 11. H0. 0 200 400 600 800. ... 100. 200. 300. 400. 0 20 40 60 80 100 120 140.

1 Jun 2006: 1. 0 100 200 300 400 Time (min). 0.6. 0.5 0. ... 38 M. G. Worster and R. C. Kerr. 300. 250. 200 n G 'g 150.

9 Feb 2004: We demonstrate that the ash-laden flow travelled over the ground in a currentof order 1 km high travelling at a typical speed of 200 m s1. ... The solid curve represents (3.26a) withβ = 0.1 andθ = 350.The dashed lines enclose the theoretical values for

13 Apr 2011: 50.0. 100.0. 150.0. 200.0. u (m. m/s. ). FIG. 5. Top left, plan form ofbeads and top right, sand flowingdown a rough inclined plane. ... 150. 200. 250. Q (g/s). u (m. m/s. ). FIG. 14.

11 Apr 2013: a) (b). 1. 1. 0. 100. 200. 101. 10 –1 100 101.

2 Jun 2015: When CDFrf t1 (for example, the solutions at t=50, 100 and 200 in figure 3a) theeffects of drag become significant.

1 Jun 2006: J. Fluid Mech. (1991), vol. 224, p p. 335-359 Printed i n Great Britain. 335. Natural convection in a mushy layer. By M. G R A E WORSTER Department of Engineering Sciences & Applied Mathematics and Department of Chemical. Engineering, Northwestern

26 Apr 2006: AR266-FL38-16 ARI 22 November 2005 19:29. Premelting DynamicsJ.S. Wettlaufer1 and M. Grae Worster21 Department of Geology and Geophysics, Department of Physics, Yale University, New Haven,Connecticut 06520-8109; email: john.wettlaufer@yale.edu2

27 Apr 2006: 8 c ) and is graphed in Fig. 5. 200 -. 160 h(m). 120. 8 0 -. 4 0 -. 107. o ,6o 26o 36o r(m). ... t f o r d i s c u s s i o n ). 0 200 400 600 Metres I i I. SCALE. Fig. 9.

25 Jan 2007: 45. 15. 0. - 5 200 400 600 800 lo00. Time (min).

26 Mar 2023: Phil. Trans.R.Soc.A 378:20200064.http://dx.doi.org/10.1098/rsta.2020.0064. Accepted: 16 March 2020. One contribution of 14 to a theme issue ‘Stokesat 200 (Part ... org. / on. 23 D. ecem. ber. 2021. 2.

23 Aug 2004: As t 0 it can be seen that the solution diverges from the line of best fit., t = 103, y = 1/200; , t = 103, y = 1/400; , t = 104, y =

9 Feb 2004: In a typical numerical integration, we used 200 grid points, a time step of 5104and an initial time oft0 = 0.5.

9 Mar 2004: The majority of the calculations have used 200 uniformlyspaced grid points in each mushy layer, although we have checked convergenceusing 400 and 800 points. ... We note that a typical calculation with 200 grid points. 178 D.

5 May 2006: 1. (a). (b). 0 50 100 150 200 250 300 350100.

21 Dec 2012: 1. 1228. 1990 2000 2010 2020 2030 2040 20500. 100. 200.

9 Mar 2004: J. Fluid Mech. (2003), vol. 489, pp. 269–299. c 2003 Cambridge University PressDOI: 10.1017/S0022112003005172 Printed in the United Kingdom. 269. Solidification and convection of a ternarysolution cooled from the side. By LYNN J. BLOOMFIELD AND

27 Apr 2006: Fig. 1. The velocity of the head is approximately constant for a distance of about 200 cm, which is approximately ten times the lock. ... 3. Over the first 1.5 m the three. 500. ' 200.

19 Jul 2010: Experimental studies of komatiite generation (Bickle et al.,1977) and thermal constraints (McKenzie, 1984) indicate depths of 200 km or greater.

30 May 2006: A. Hallworth. I I I 0 50 200 300 400 500. ... Time (min). I. 0 50 200 300 400 500. Time (min).

19 Jul 2010: 2.1. Experimental techniques. The experiments were carried out in a cubical Perspex tank measuring 200 mm on eachside internally, which was insulated with a 90 mm thick polystyrene jacket (removable

16 Jan 2007: 0 400 800 1200 t (min). 1600. -8 I 1 I I I 0 200 400 600 800.