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Publications
www.itg.cam.ac.uk/people/grae/publications.html8 Jul 2024: 24. Wettlaufer, J.S. & Worster, M.G. 1995. Dynamics of premelted films: frost heave in a capillary. ... Physics of Fluids, 24, 091111. -
Tuesday Informal Lunch Seminars
www.itg.cam.ac.uk/seminars/tue_1.10/lent_2004.html10 Feb 2004: 24 February. Steve Roper. (ITG). Magma fracture in tough materials. 2 March. -
Dr. Anneli Aitta
www.itg.cam.ac.uk/people/aa/10 May 2011: I. Taylor, 24-28 March 1986, Cambridge, U.K. My third main research project has been on the statics and dynamics of symmetry breaking when it changes from being forward to -
Thursday Seminars on Theoretical Geophysics
www.itg.cam.ac.uk/seminars/thu_2.05/mich_2005.html23 Nov 2005: 24 November. Peter Challenor. (Southampton). Wave climate from space -- from Geosat to Hurricane Katrina. -
Tuesday Informal Lunch Seminars
www.itg.cam.ac.uk/seminars/tue_1.10/mich_2009.html5 Oct 2009: 17 November. APS practice talks. 24 November. APS meeting - no seminar. -
Thursday Seminars on Theoretical Geophysics
www.itg.cam.ac.uk/seminars/tue_1.10/mich_2002.html9 Apr 2003: 17 October. Ian Main. (Edinburgh). Statistical physics of earthquake populations. 24 October. -
Tuesday Informal Lunch Seminars
www.itg.cam.ac.uk/seminars/tue_1.10/lent_2006.html24 Jan 2006: Please bring your own lunch. 24 January. Thibaut Putelat. (ITG). On the selection of active fault planes. -
Thursday Seminars on Theoretical Geophysics
www.itg.cam.ac.uk/seminars/thu_2.05/lent_2011.html17 Jan 2011: 24 February. MR9. Thierry Alboussiere. (ENS Lyon). The 'not so quiet' inner core. -
doi:10.1016/j.jcrysgro.2008.04.046
www.itg.cam.ac.uk/people/heh/Paper212.pdf7 Aug 2008: Article history:. Received 8 February 2008. Received in revised form. 24 April 2008. ... When solidifying 24 wt% NH4Cl at the lower temperaturegradient we observed another regime in which chimneys and. -
The effect of confining boundaries on viscous gravity currents
www.itg.cam.ac.uk/people/heh/Paper201.pdf8 May 2007: 2(m2 1). 2u. XY= Mm2h2. (2.24). We posit a solution in the form. ... 4.1) for openchannel flow is replaced by 24/105 = 0.229 for a circular constraining geometry andK/m = 0.137m2/(1 m2) for a V-shaped constrainer. -
jc004333 1..7
www.itg.cam.ac.uk/people/grae/82.pdf7 Aug 2008: During the rapid development ofthe initial very thin ice, most of the salt is lost within 24 h.In the slower-growing ice the desalination rate is muchsmaller, and it takes ... 24] Acknowledgments. The field work described in this paperwould not have been -
gl044728 1..5
www.itg.cam.ac.uk/people/heh/Paper223.pdf13 Apr 2011: Huppert1. Received 17 July 2010; revised 23 September 2010; accepted 27 September 2010; published 24 November 2010. -
Lee waves in a stratified flow Part 3. Semi-elliptical obstacle
www.itg.cam.ac.uk/people/heh/Paper8.pdf30 May 2006: a$'(@, SY), DPI = { P } [ 1 , 1 , S&I, (4.23) where yil) = P-1Bi/Ms$2) (4.24 a). ... 4.24 b) = 1 1 8 ) K21og K O ( K 2 ). Truncating a t n = N = 2 , we obtain the second approximation. -
PII: 0022-0248(93)90538-8
www.itg.cam.ac.uk/people/heh/Paper116.pdf27 Apr 2006: iments havebeenusedin drawing up fig. 3.) Fig.1 • 24.5 5 then plots the heightsof the mushy layer and. ... 0 24 concentrationsas functions of time for experi-0 100 200 300 400 500 mentswith the six different valuesof the contam-. -
J. Fluid Mech. (2022), vol. 931, A12, doi:10.1017/jfm.2021.944…
www.itg.cam.ac.uk/people/heh/Paper284.pdf26 Mar 2023: 6.8)Substituting (6.8) and (6.3) into (6.4), we obtain. w2N /(24 tan2 α) sN wN = 3A/2, wN =. (vN. β sin α. )1/2,. wN = 12 tan -
1-s2.0-S1359645418304166-main
www.itg.cam.ac.uk/people/grae/You.pdf17 Jan 2019: With these scalings, equations(22) and (24) can be written in dimensionless form as. ... 24] A.W. Rempel, M.G. Worster, The interaction between a particle and anadvancing solidification front, J. -
flm1100071a
www.itg.cam.ac.uk/people/heh/Paper228.pdf21 Oct 2011: 546 A. C. Slim and H. E. Huppert. curve having. F (3 24/3Mr /7. ... B. 1996 Mixing in lock-release gravity currents. Dyn. Atmos.Oceans 24, 183–195. -
PII: S0022-0248(99)00456-X
www.itg.cam.ac.uk/people/grae/42.pdf26 Apr 2006: The boundaryconditions at t'0 are Eq. (12),. h"0 (z"f(t)) (23). [h]ml "0 (z"f(t)), (24). ... Wettlaufer, M.G. Worster, H.E. Huppert, Geophys. Res. Lett. 24 (1997) 1251.[12] D.L. -
Inclined gravity currents filling basins: The influence of Reynolds…
www.itg.cam.ac.uk/people/heh/Paper253.pdf30 Oct 2015: C. Christodoulou, “Interfacial mixing in stratified flows,” J. Hydraul. Res. 24, 77–92 (1986).4 B. ... Downloaded. to IP: 131.111.16.57 On: Fri, 30 Oct 2015 10:24:16. -
PII: S0022-0248(01)00595-4
www.itg.cam.ac.uk/people/grae/45.pdf26 Apr 2006: 24),so f! 0 as x! 1. The interface shape is deter-mined from the equation for f in the inner regionalone. ... Wettlaufer, Rep. Prog. Phys. 58. (1995) 115. [24] J.S. Wettlaufer, M.G. -
Under consideration for publication in J. Fluid Mech. 1 ...
www.itg.cam.ac.uk/people/heh/jfm50.pdf28 Jul 2006: Geology 186 24.6 1.64 220 12.6 1.80. JFM 197 22.5 1.50 265 11.3 1.61. -
85230
www.itg.cam.ac.uk/people/heh/Paper146.pdf27 Apr 2006: 15, p. 9–24. Eppler, D. B., Fink, J., and Fletcher, R., 1987, Rheologic properties and kinematics ofemplacement of the Chaos Jumbles rockfall avalanche, Lassen Volcanic NationalPark, California: Journal of Geophysical -
M411_31c 568..571
www.itg.cam.ac.uk/people/grae/47.pdf27 Apr 2006: 24. Zielinski, G. A. Use of paleo-records in determining variability within the volcanism-climate system. -
doi:10.1098/rspa.2006.1790
www.itg.cam.ac.uk/people/grae/77.pdf22 Jan 2007: Inserting equations (2.23) and (2.24) into equations (2.12)–(2.16) andlinearizing in the perturbed quantities leads to the following nonlinear ordinarydifferential equation for the disturbance amplitude:. -
PHYSICAL REVIEW E 83, 031306 (2011) Shallow granular flows ...
www.itg.cam.ac.uk/people/heh/Paper226.pdf13 Apr 2011: 24. The wave speed c is scaledby. ghstop cos θ and the maximal thickness hf by hstop. ... Jop, Y. Forterre, and O. Pouliquen, Nature (London) 441, 727. (2006).[24] I. -
J. Fluid Mech. (2014), vol. 753, R1, doi:10.1017/jfm.2014.395…
www.itg.cam.ac.uk/people/heh/Paper248.pdf21 Nov 2014: 19:. 20:. 21:. 22:. 23:. 24:. 25:. 26:. 27:. 28:. 29:. -
J. Fluid Mech. (2019), vol. 874, pp. 285–298. c© ...
www.itg.cam.ac.uk/people/heh/Paper268.pdf23 Dec 2021: Thus,with 1ρ =ρ because the density of the overlying air can be neglected, β = 24.8 or0.295 cm1 s1 and (βV 1/3)1 was between 0.004 s ... A 24). Dow. nloa. ded. from. htt. ps://. ww. w.c. ambr. -
rspa.royalsocietypublishing.org ResearchCite this article: Cooray H,…
www.itg.cam.ac.uk/people/heh/Paper255.pdf18 May 2017: x = h(y) = 16 y3 c1y c2, (4.24)where c1 and c2 are constants. ... angles. SIAM J. Appl. Math. 49, 1009–1028. (doi:10.1137/0149061)24. Vogel TI. 2013 Liquid bridges between balls: the small volume instability. -
J. Fluid Mech. (2016), vol. 802, pp. 750–759. c© ...
www.itg.cam.ac.uk/people/heh/Paper256.pdf18 May 2017: 1γ). 1H(L). (p11/γD p11/γS. )(2.23). (. γ. 1γ). 1H(L). p11/γD. (2.24). -
Theoret. Comput. Fluid Dynamics (1998) 10: 201–212Theoretical and…
www.itg.cam.ac.uk/people/heh/Paper140.pdf9 Feb 2004: r = (F/πV )1/2. (2.24)In contrast to the instantaneous, fixed volume release of the last section, there is not a finite radius at whichthe mass of particulate matter ... Applying these concepts to the relationship for the density of deposit for a single -
doi:
www.itg.cam.ac.uk/people/heh/Paper240.pdf14 Feb 2013: 22:. 23:. 24:. 25:. 26:. 27:. 28:. 29:. 30:. 31:. 32:. -
PHYSICAL REVIEW E 84, 036111 (2011) Elastic response of ...
www.itg.cam.ac.uk/people/grae/98.pdf24 Aug 2012: 0.1. 0 10. 0. 0.4. 101108. x/l0 10. 0. 0.4. S = 3 S = 24. ... σxx = E(1 ν)(1 2ν) [(1 ν)xx νyy ],. σyy = E(1 ν)(1 2ν) [(1 ν)yy νxx ], (24). -
flm021.dvi
www.itg.cam.ac.uk/people/heh/Paper209.pdf14 May 2008: 21. 22. 23. 24. 25. 26. 27. 28. V (µm s–1). -
flm145.dvi
www.itg.cam.ac.uk/people/heh/Paper197.pdf11 Oct 2006: After some algebra and use of(2.24), we obtain. ρD. Dt. [1. ... 374 M. Ungarish and H. E. Huppert. t0 4 8 12 16 20 24. -
2000JC000559
www.itg.cam.ac.uk/people/grae/55.pdf26 Apr 2006: Leppäranta, pp. 24–104,Univ. of Helsinki Press, Helsinki, 1998. Wettlaufer, J. S., Heat flux at the ice-ocean interface, J. ... E. Huppert, The phase evolution ofyoung sea ice, Geophys. Res. Lett., 24, 1251–1254, 1997a. -
J. Fluid Mech. (2022), vol. 932, A5, doi:10.1017/jfm.2021.963 The ...
www.itg.cam.ac.uk/people/heh/Paper285.pdf26 Mar 2023: as. th/T = 0.63, (2.24)at which time rN /L = 0.92 and h/L = 0.67. ... Illustrative evaluations of the time scales on which the axisymmetric transition from radial tothin-layer regimes occurs, given by (2.21)–(2.24), for a selection of geological -
Ice growth in a spherical cavity of a porous ...
www.itg.cam.ac.uk/people/grae/96.pdf10 Mar 2011: MS received 24 June 2009 and accepted in revised form 10 February 2010. -
Stokes, Tyndall, Ruskin and the nineteenth-century beginnings of…
www.itg.cam.ac.uk/people/heh/Paper271.pdf26 Mar 2023: So, was Ruskin simply blaming air pollution on the devil? Ruskin’s biographer notes the fact that[24]. -
PHYSICAL REVIEW E 87, 023015 (2013) Interface pinning of ...
www.itg.cam.ac.uk/people/heh/Paper239.pdf11 Apr 2013: In a related context, the classical modelhas been modified to replace the sharp interface by a capillarytransition zone [24–26]. ... Porous Media 18, 107 (1995).[24] L. W. Lake, Enhanced Oil Recovery (Prentice-Hall, Englewood. -
PHYSICAL REVIEW E 93, 023116 (2016) Flow-induced compaction of ...
www.itg.cam.ac.uk/people/grae/120.pdf21 Mar 2016: Received 24 June 2015; revised manuscript received 1 January 2016; published 24 February 2016). ... 24)] while the effective permeability decreases like H1(cf. (22)). The porosity also approaches an asymptotic profilewith φ0 0 as H. -
Some remarks on the initiation of inertial Taylor columns
www.itg.cam.ac.uk/people/heh/Paper19.pdf30 May 2006: r 2 ) ( r < 1) 2.94 0.93 1.27 1.00 {(‘i ( r > 1 ). - I Cylindrical Gaussian e-T2 ( f < 00) 3.13 1-12 2.24 0.86. ... If h,R-l > Fmin (2.24) t It is interesting to compare these values with the relationship h0R-l = 2 deduced by. -
doi: 10.1098/rspa.2009.0496, 1005-1025 first published online 3…
www.itg.cam.ac.uk/people/grae/91.pdf29 Apr 2010: we can make the approximation G(y) π y. Equation (2.24) then becomesπ. ... By dimensionalization of equation (3.24), we findthat the system is stable when. -
PII: 0022-0248(94)90038-8
www.itg.cam.ac.uk/people/grae/22.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)—. -
flm608.dvi
www.itg.cam.ac.uk/people/heh/Paper177.pdf9 Mar 2004: 6.3 6.3 24.3 5.89 1.00 3.86 9.6 6.1 3.8 0.7417 6.3 6.3 24.3 10.71 1.00 ... 86 9.6 8.2 5.2 0.8118 6.3 6.3 24.3 20.37 1.00 3.86 9.6 11.3 7.1 0.8919 13.2 -
Experiments on the low-Reynolds-number settling of a sphere through a …
www.itg.cam.ac.uk/people/heh/Paper265.pdf23 Dec 2021: seal” configurations observed for inertial impacts of spheres ontoair-water [24] and fluid-fluid [26] interfaces. ... Phys. 3, 180. (2007).[23] D. Lee and H. Kim, Impact of a superhydrophobic sphere onto water, Langmuir 24, 142 (2008).[24] J. -
The propagation of two-dimensional and axisymmetric viscous gravity…
www.itg.cam.ac.uk/people/heh/Paper47.pdf30 May 2006: 2.21). (2.22). (2.23). (2.24). where EN is the value of [ at r = rN(t). ... Substituting (2.23) and (2.24) into (2.21) and (2.22), we find that $ ( z ) , where z = c/&, satisfies. -
Viscous free-surface flows past cylinders
www.itg.cam.ac.uk/people/heh/Paper274.pdf26 Mar 2023: The governing Eq. (7) in the rescaledcoordinates is. h3. x̂=. [. x̂. (h3. h. x̂. ). ŷ. (h3. h. ŷ. )]. (24). ... 5.0 24 15 7.14 1.2 0.853.5 48 13.2 4.50 1.72 0.615.0 24 7.9 3.76 1.28 0.773.5 -
PII: 0011-7471(73)90056-9
www.itg.cam.ac.uk/people/heh/Paper15.pdf26 Sep 2011: 24). F o r a solution to be possible the right-hand side o f (24) must be positive, that is (with Yr negative). -
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. -
Initial advance of long lava flows in open channels
www.itg.cam.ac.uk/people/heh/Paper222.pdf27 Aug 2010: However, variations in fountain height in episode 4, asplotted in figure 1.24 of Wolfe et al. ... the night of 24–25 July 1983,when the flow front divided into two parallel lobes.
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