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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.

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

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

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.

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.

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

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

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. )