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6 Jun 2024: 24. Wettlaufer, J.S. & Worster, M.G. 1995. Dynamics of premelted films: frost heave in a capillary. ... Physics of Fluids, 24, 091111.

10 Feb 2004: 24 February. Steve Roper. (ITG). Magma fracture in tough materials. 2 March.

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

23 Nov 2005: 24 November. Peter Challenor. (Southampton). Wave climate from space -- from Geosat to Hurricane Katrina.

5 Oct 2009: 17 November. APS practice talks. 24 November. APS meeting - no seminar.

9 Apr 2003: 17 October. Ian Main. (Edinburgh). Statistical physics of earthquake populations. 24 October.

24 Jan 2006: Please bring your own lunch. 24 January. Thibaut Putelat. (ITG). On the selection of active fault planes.

17 Jan 2011: 24 February. MR9. Thierry Alboussiere. (ENS Lyon). The 'not so quiet' inner core.

7 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.

8 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.

7 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

13 Apr 2011: Huppert1. Received 17 July 2010; revised 23 September 2010; accepted 27 September 2010; published 24 November 2010.

30 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.

26 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

27 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-.

17 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.

26 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.

21 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.

28 Jul 2006: Geology 186 24.6 1.64 220 12.6 1.80. JFM 197 22.5 1.50 265 11.3 1.61.

27 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

26 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.

27 Apr 2006: 24. Zielinski, G. A. Use of paleo-records in determining variability within the volcanism-climate system.

30 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.

22 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:.

21 Nov 2014: 19:. 20:. 21:. 22:. 23:. 24:. 25:. 26:. 27:. 28:. 29:.

23 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.

13 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.

18 May 2017: 1γ). 1H(L). (p11/γD p11/γS. )(2.23). (. γ. 1γ). 1H(L). p11/γD. (2.24).

9 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

14 Feb 2013: 22:. 23:. 24:. 25:. 26:. 27:. 28:. 29:. 30:. 31:. 32:.

18 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.

24 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).

14 May 2008: 21. 22. 23. 24. 25. 26. 27. 28. V (µm s–1).

26 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.

26 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

11 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.

10 Mar 2011: MS received 24 June 2009 and accepted in revised form 10 February 2010.

26 Mar 2023: So, was Ruskin simply blaming air pollution on the devil? Ruskin’s biographer notes the fact that[24].

11 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.

30 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.

21 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.

27 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)—.

29 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.

23 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.

30 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.

9 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

26 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).

27 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.

26 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

18 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.