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High Reynolds number gravity currents along V-shaped valleys
www.itg.cam.ac.uk/people/heh/Paper217.pdf18 Nov 2009: y1=2ð1 þ yÞ1=2ln. y1=2 þffiffiffiffiffiffiffiffiffiffiffiffi1 þ y. p s þ c1; (24). ... Am.Math. Soc. 46 (1940) 615–683. [24] T.B. Benjamin, Gravity currents and related phenomena, J. -
The Fluid Mechanics of Carbon Dioxide Sequestration
www.itg.cam.ac.uk/people/heh/Paper246.pdf24 Apr 2014: 24/. 14. F. or p. erso. nal u. se o. nly. ... n 04. /24/. 14. F. or p. erso. nal u. se o. -
Ageostrophic effects in rotating stratified flow
www.itg.cam.ac.uk/people/heh/Paper17.pdf30 May 2006: 24-2. 372 H. E. Huppert and 144. E. Stern. $1. , //,/,////,//////////////,,,/,////// / ///,/I/ // / / / , // , / , / // , / / / / // / /, /' I -. FIGURE 1. An elevation of the channel, bounded by vertical walls at. ... Moh(x/L) e--ikg. (3.24). While in -
doi:10.1016/j.jcp.2004.11.039
www.itg.cam.ac.uk/people/grae/62.pdf26 Apr 2006: Received 29 March 2004; received in revised form 24 September 2004; accepted 11 November 2004. ... ykumar and Mao [24] again assuming the interface was sharp. The SPH method, as mentioned earlier, does. -
PII: 0022-0248(94)90038-8
www.itg.cam.ac.uk/people/heh/Paper119.pdf27 Apr 2006: 2.18), which can be (2.23) and (2.24) more closely.used in (2.22) to show that Segregation is more sensitive to the value of. ... 4.24)mass reduce to and we use this condition together with (4.21)—. -
PII: S0022-0248(99)00290-0
www.itg.cam.ac.uk/people/grae/40.pdf26 Apr 2006: 1.0 [24]. The slope of the linethrough data set (h), for silicon carbide particles in a succino-nitrile melt, is! ... Azouni, W. Kalita, M. Yemmou, J. Crystal Growth. 99 (1990) 201.[24] S. -
Laminar free convection in confined regions
www.itg.cam.ac.uk/people/grae/4.pdf1 Jun 2006: 1 -. f = 16-21 min. 24.5 25.0 25.5 26.0 26.5 27.0 27.5 28.0 28.5 29.0 T. ... 0 - 1 24.5 25.0 25.5 26.0 26.5 27.0 27.5 28.0 28.5 29.0 29.5 30.0 30.5. -
flm1000491a
www.itg.cam.ac.uk/people/heh/Paper225.pdf18 Jan 2011: φ̃0(0; λ̄) =. h(0, y)2 dy. (3.24). The solid curve in figure 5 shows the result of substituting the value of φ̃0(0; λ̄)found in this way -
doi:10.1016/j.jcp.2005.12.002
www.itg.cam.ac.uk/people/grae/74.pdf12 Jun 2006: g. [23,24]). The major difficulties then consist in the formulation of accurate internalboundary conditions and in following the evolution of the interfaces through time. ... 104 This study 19.6 16.2 3.53 0.585 2.24[2] 19.51 16.2 3.53 0.586 2.243[3] -
Thermohaline Steps Induced By Melting of the Erebus Glacier Tongue
www.itg.cam.ac.uk/people/heh/Paper44.pdf16 Jul 2010: Geophys. Res., 79, 1792-1797, 1974. Gebhart, B., and J. C. Molendorf, A new density relationship for pure and saline water, Deep Sea Res., 24(9), 831-848, 1977. ... Glaciol., 24, 259-271, 1979. Tressler, W. L., and A.M. Ommundsen, Seasonal oceanographic
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