Search
Search Funnelback University
51 -
100 of
202
search results for katalk:za33 24 |u:www.itg.cam.ac.uk
where 0
match all words and 202
match some words.
Results that match 1 of 2 words
-
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. -
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 -
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. -
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 -
PII: S0301-9322(98)00062-7
www.itg.cam.ac.uk/people/heh/Paper151.pdf9 Mar 2004: rNt 0 rN0 24. M. Ungarish, H.E. Huppert / International Journal of Multiphase Flow 25 (1999) 715737 725. ... For this case. the box model yields [rN/rN(0)]max=[8Fr/(3 b)]1/4. (This is by about 24% smaller than for. -
J. Fluid Mech. (2015), vol. 777, pp. 97–121. c© ...
www.itg.cam.ac.uk/people/heh/Paper252.pdf30 Oct 2015: leakage rate predicted by (2.24) is then unphysical because there is no fluidabove the outlet to draw. ... Generally, this assumptionis invalid if the current delivers a smaller flux towards the outlet than is predicted toleak according to (2.24). -
Nonlinear double-diffusive convection
www.itg.cam.ac.uk/people/heh/Paper25.pdf30 May 2006: J. F u i d Xech. (19761, VOZ. 78, part 4? pp. 821-854 Printed in Great Britain. 82 1. Nonlinear double-diffusive convection By H E R B E R T E. H U P P E R T A N D D A N I E L R. MOORE. Department of Applied Mathematics and Theoretical Physics, -
doi:10.1016/j.jcp.2004.11.039
www.itg.cam.ac.uk/people/heh/Paper187.pdf5 May 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. -
jc001173 1..12
www.itg.cam.ac.uk/people/grae/57.pdf26 Apr 2006: Using equations (3) and (22)–(24), it is possibleto calculate _h, S0 and T0 in terms of far-field properties T1and S1 by eliminating two of the unknowns to obtain aquadratic ... For this simula-tion we used again the values given in Table 1 and Si = -
Instruments and Methods A non-destructive method for measuring the ...
www.itg.cam.ac.uk/people/grae/61.pdf28 Apr 2006: InArctic sea ice. Conference held at Easton, Maryland, February 24–27, 1958. -
Tuesday Informal Lunch Seminars
www.itg.cam.ac.uk/seminars/tue_1.10/mich_2006.html17 Oct 2006: Exchange flows during the ventilation of buildings. 24 October. Richard Katz. -
Dynamics of viscous grounding lines
www.itg.cam.ac.uk/people/heh/Paper220.pdf6 May 2010: H. t+. q. x= 0 (2.24). to form the nonlinear diffusion equation. ... f (ξ ) dξ = 1, (3.24). to the leading-order front solution (3.21). -
Thursday Seminars on Theoretical Geophysics
www.itg.cam.ac.uk/seminars/thu_2.05/lent_2005.html18 Feb 2005: 24 February. Chris Chapman. (Schlumberger). Marine seismics with a rough sea: modelling the surface reflection. -
jc002818 1..17
www.itg.cam.ac.uk/people/grae/66.pdf27 Apr 2006: Received 24 November 2004; revised 19 May 2005; accepted 11 August 2005; published 2 February 2006. ... The wider range of melt rates were used toexamine model sensitivity to mi.[24] In an extensive study of four sea ice sites in the. -
rsta.royalsocietypublishing.org ResearchCite this article: Worster…
www.itg.cam.ac.uk/people/grae/117.pdf9 Oct 2015: Although sea water with salinity above approximately 24 ppt has a monotonic variation ofdensity with temperature above its freezing temperature, the same physics that gives rise to thedensity maximum of pure -
The slumping of gravity currents
www.itg.cam.ac.uk/people/heh/Paper32.pdf30 May 2006: head. This Froude number should be 24 according to Benjamin, but Hoult suggests expressing it as a constant A, to be determined from experiment. -
PHYSICS OF FLUIDS VOLUME 13, NUMBER 12 DECEMBER 2001 ...
www.itg.cam.ac.uk/people/heh/Paper167.pdf9 Feb 2004: H 0 1!5 2F P12 f P1 1! 4.24! FIG. 2. ... On applicationthe boundary conditions4.23! and 4.24!, we find that. a 5 4.523 102 3, F P15 2 8.42 for Fr5 11.9. -
J. Fluid Mech. (2002), vol. 458, pp. 283–301. c© ...
www.itg.cam.ac.uk/people/heh/Paper171.pdf9 Mar 2004: These substitutions transform (2.24) into. uN = I(hN) = Fr(hN) h1/2N. ... Appendix. The functions I and χA.1. The function I(hN). From the definitions (2.19), (2.24) and (2.25) we obtain. -
J. Fluid Mech. (2018), vol. 844, pp. 435–458. c© ...
www.itg.cam.ac.uk/people/heh/Paper263.pdf23 Dec 2021: 2.24). Using these dimensionless groups, we introduce the viscosity- and toughness-dominated scalings, denoting them with subscripts m and k, respectively. ... balance (2.24) to obtain the radial scaling,. Rk =. (Q2E′2t2. K′2. -
PII: 0012-821X(81)90075-3
www.itg.cam.ac.uk/people/heh/Paper43.pdf16 Jan 2007: expressed as wt.%, as a function of the amount of K2CO 3 or NaNO 3 present in solution at 24.2C. ... Lower and upper layer properties were: initial temperatures 46 and 15C; initial concentrations 37 and 24%; initial densities 1.26 and 1.23 g cm 3; and -
The effect of side walls on homogeneous rotating flow over…
www.itg.cam.ac.uk/people/heh/Paper18.pdf30 May 2006: The situation can be made to appear even more problematic by continuing the analysis further, (2.24)-(2.31), from which i t appears that a full, three-dimensional calculation, incorporating ... 2 [ M o ( [ ) u(l)([)Ir 2 4 v ( ) ” ( [ ) 24. -
J. Fluid Mech. (2001), vol. 432, pp. 201–217. Printed ...
www.itg.cam.ac.uk/people/aa/JFM1.pdf9 Mar 2004: 15 P 24.2 P25.2 L25.2 P25.2 P30.2 L. T (C) T (C). -
Ice blocks melting into a salinity gradient
www.itg.cam.ac.uk/people/heh/Paper35.pdf30 May 2006: 0 69.5 24.6 30.4 40.8 47.3 62-5 29.2 37.2 51.9 41.7 23.7 29.7 36.5 42.2. ... 29.6 36.6 25.0 34.8 54.0 24.8 33-8 28.2 35.3 24.3. 1 0 3 dp. -
Replenishment of Magma Chambers by Light Inputs
www.itg.cam.ac.uk/people/heh/Paper70.pdf19 Jul 2010: Petrol., 24, 133-165, 1983. Eichelberger, J. C., Vesiculation of mafic magma during replenish- ment of silicic magma reservoirs, Nature, 288, 446-450, 1980. -
Static and flowing regions in granular collapses down…
www.itg.cam.ac.uk/people/heh/Paper208.pdf13 Nov 2007: Method. Glass beads 24 Rotating drume. 0.25–0.35 24 Smooth inclined planef. ... 0.5 0.04 24–31 Rough inclined planeg. 1.26 9–11 Shear gauge, smooth chute flowh. -
Flow and instability of thin films on a cylinder and sphere
www.itg.cam.ac.uk/people/heh/Paper219.pdf6 May 2010: where representative valuesof ρ = 1.4 kg m3, g = 9.8 m s2, γ = 78 mN m1 and R = 0.24 m were fixed. ... and R = 0.24 m. Wavelengths were estimated by dividing the circumference of the leading edgeof the flow at the onset of instability by the number of -
Gravitational and buckling instabilities of a rheologically layered…
www.itg.cam.ac.uk/people/heh/Paper169.pdf19 Jul 2010: η1. )w2(0),. (24). (. 1. k2D3 D. )w1(0) η2. η1. (1. -
Viscous gravity currents inside confining channels and…
www.itg.cam.ac.uk/people/heh/Paper210.pdf5 Mar 2008: Received 30 October 2007; accepted 24 January 2008; published online 29 February 2008. -
The growth and structure of double-diffusive cells adjacent to a…
www.itg.cam.ac.uk/people/heh/Paper183.pdf5 May 2006: 24 48.2 20.9 26 120 0.83 2.6 1760 2.7 1.38 48.2 20.5 20.3 20 1.18 1.5 2250 2.1 ... 34. 32. 30. 28. 26. 24. 22. 20. 18. 16. 14. -
Hogg, Charlie A. R., Clelia L. Marti, Herbert E. Huppert, and…
www.itg.cam.ac.uk/people/heh/Paper238.pdf12 Apr 2013: Parameter Value. Inflow channel width (m) 49Inflow channel depth (m) 1.7Inflow velocity (m s21) 0.48Inflow reduced gravity (m s22) 0.021Inflow temperature (uC) 13.0Lake surface temperature (uC) -
la303458m 1..12
www.itg.cam.ac.uk/people/grae/103.pdf9 Apr 2013: These colloidal concentration gradients, which areneglected in rigid-ice formulations, can trigger a thermody-namic instability that leads to morphological transitions in thepattern of segregated ice.23,24 Recently, these thermodynamicprinciples -
Collapses of two-dimensional granular columns Gert Lube,1 Herbert E.…
www.itg.cam.ac.uk/people/heh/Paper190.pdf5 May 2006: www.damtp.cam.ac.uk/lab/digiflow/ 2005.23 G. S. Campbell, Annu. Rev. Fluid Mech. 22, 57 1990.24 T. -
PII: 0377-0273(93)90087-8
www.itg.cam.ac.uk/people/heh/Paper110.pdf27 Apr 2006: Subsequently (ap- proximately 40-50 rain from the beginning),. 24 r. KOYa_GUCHI L, kt. ... grade particles with A T = 2 4 C and Co= 1.24 wt.%. -
Solidification of an alloy cooled from above. Part 3. Compositional…
www.itg.cam.ac.uk/people/grae/11.pdf1 Jun 2006: E. Huppert. Parameter Value Units. a (5.0+ 0.24( T- 20)) x U 0.015 cm2 s-' CC 4.14 J O C - '. 2.66 J cm-3 O C - ' -
Using PHF format
www.itg.cam.ac.uk/people/heh/Paper150.pdf9 Feb 2004: The volume fration of particles in suspension evolves as23,24. df. dt5. ... X5 x/l , 24! T5 t/ v sl /q!1/ a 2 1!, 25! -
J. Fluid Mech. (2001), vol. 432, pp. 201–217. Printed ...
www.itg.cam.ac.uk/people/heh/Paper159.pdf9 Mar 2004: 15 P 24.2 P25.2 L25.2 P25.2 P30.2 L. T (C) T (C). -
jc004885 1..10
www.itg.cam.ac.uk/people/grae/89.pdf14 Sep 2009: is in the direction of rT).[24] Typical advection velocities estimated from a tem-. ... Assur, A. (1958), Composition of sea ice and its tensile strength, in ArcticSea Ice; Conference Held at Easton, Maryland, February 24–27, 1958,pp. -
PII: S1359645497004692
www.itg.cam.ac.uk/people/heh/Paper144.pdf12 Mar 2004: requires. P q02pd. : 24. Equation (24) thus links the dendrite tip radius to. ... This solution has a scaled tip radius P = 10.8. and a scaled tip position Z 2:24. -
flm903.dvi
www.itg.cam.ac.uk/people/heh/Paper180.pdf10 Jun 2004: a. r – riri. sandsaltricecouscoussugar slope 1.24. Figure 9. The non-dimensional radial excursion, (r ri )/ri , as a function of the aspect ratioa with a < 1.7 for sand, salt, ... A straight line through the origin atslope 1.24 has a regression -
Assessment of ice flow dynamics in the zone close to the calving…
www.itg.cam.ac.uk/people/grae/118.pdf21 Mar 2016: Assessment of ice flow dynamics in the zone close to the calvingfront of Antarctic ice shelves. Martin G. WEARING,1;2 Richard C.A. HINDMARSH,1 M. Grae WORSTER2. 1British Antarctic Survey, Natural Environment Research Council, Cambridge, -
Handbook of Environmental Fluid Dynamics: Overview and Fundamentals
www.itg.cam.ac.uk/people/grae/104.pdf9 Apr 2013: 2 2 2. 24/.467. 35.1 Introduction. -
J. Fluid Mech. (2000), vol. 418, pp. 1–23. Printed ...
www.itg.cam.ac.uk/people/heh/Paper155.pdf9 Mar 2004: Indeed, for most of the experimentsdiscussed by TML λ was in the range 0.02–0.24. ... tr dr rN. drNdthN. (2.24). We eliminate h/t with the aid of (2.12) and, after some rearrangement, we againobtain the result (2.22). -
Solidification of leads: Theory, experiment,and field observations J. …
www.itg.cam.ac.uk/people/grae/43.pdf26 Apr 2006: salinity of the ice) is very small; k #1 0 24 [Gross et al., 1987]. -
flm1100021a
www.itg.cam.ac.uk/people/heh/Paper227.pdf21 Oct 2011: The camera was operated at 1000 frames s1. and a resolution of 640 512 pixels (24 bits). ... 18.8 cm. 24.7 cm. 31.1 cm. 37.6 cm. 43.3 cm. 49.7 cm. -
Solidification of an alloy cooled from above. Part 3. Compositional…
www.itg.cam.ac.uk/people/heh/Paper95.pdf25 Jan 2007: E. Huppert. Parameter Value Units. a (5.0+ 0.24( T- 20)) x U 0.015 cm2 s-' CC 4.14 J O C - '. 2.66 J cm-3 O C - '
Search history
Recently clicked results
Recently clicked results
Your click history is empty.
Recent searches
Recent searches
Your search history is empty.