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17 Feb 2009: 17 February. Jian Du. (DAMTP). Tides in the middle Atmosphere. 24 February.

5 Mar 2008: 24 January. Nick Arndt. (LGCA, Universite J. Fourier). Thermal evolution of the Earth: evidence from Archean komatiites and basalts.

9 Mar 2004: Sm =. 0. (ni=1. ψi(0) exp (2Viy))1/2. dy. (2.24). Recall thatn. ... 1 = 2/H0. (3.24)Hence from (3.16), by forming an expansion for ϕi, we find that.

19 Jul 2010: Komatiites II: Experimental and Theoretical. Investigations of Post-emplacement. Cooling and Crystallization. by J. STEWART TURNER,1 HERBERT E. HUPPERT,2 ANDR. STEPHEN J. SPARKS3. 1 Research School of Earth Sciences, Australian National University,

9 Mar 2004: J. Fluid Mech. (2003), vol. 497, pp. 167–199. c 2003 Cambridge University PressDOI: 10.1017/S002211200300661X Printed in the United Kingdom. 167. Solidification and compositional convectionof a ternary alloy. By ANDREW F. THOMPSON†, HERBERT E.

20 Jan 2023: a total of over 24,000 citations and an h index of 83 (according to Google Scolar). ... Res. Lett. 24, 1251-54.

30 May 2006: J. Fluid Me&. (1981), vol. 106, p p. 299-329. Printed in Great Britain 399. Double-diffusive convection. By H E R B E R T E. H U P P E R T Department of Applied Mathematics and Theoretical Physics,. Silver Street, Cambridge CB3 9EW. A N D J. S T E W

27 Apr 2006: 1034 23.0 24.0 0.016 67. K 1.3 w t. % saline s o l u t i o n S e d i m e n t m ... 1034 24.0 10.0 0.012 28. L 1.3 wt.% saline s o l u t i o n Secliment m fresh w a t e r.

25 Jan 2007: Substituting (18), (19) and (24) into (21), we obtain the following implicit relationship between T and Tl :. ( 2 5 ). Substituting (20) and (21) into ( 2 2 ) , and using (23a, c ) in ... a = pcDH;' (To--T). (24). Tl = Tmp2c2k' D J H i l ( T o - T ) (T-T,

9 Mar 2004: salinity of the ice) is very small; k #1 0 24 [Gross et al., 1987].

30 May 2006: J. Fluid Mech. (1995), vol. 289, p p. 263-293 Copyright 0 1995 Cambridge University Press. 263. Sedimentation and entrainment in dense layers of suspended particles stirred by an oscillating grid. By H E R B E R T E. HUPPERT', J. STEWART TURNER' A N

27 Apr 2006: r N = c ( ) (gS3/3v) 118 t (3 I)18 (2.24). ... 8 a n d using (2.24}. The results are:. S = 0.

9 Nov 2017: Falling plumes of point particles in viscous fluid. Phys. Fluids 24, 123101.

18 Sep 2001: Czech Republic and ITG). Convective instability of bubbly layers. 24 October.

9 Apr 2013: Fluids 24, 091111 (2012); doi: 10.1063/1.4747184 View online: http://dx.doi.org/10.1063/1.4747184 View Table of Contents: ... 091111-2 Sayag, Pegler, and Worster Phys. Fluids 24, 091111 (2012). (b) (c).

26 Mar 2023: 23, John Lister; 24, Colm Caulfield; 25, John Bush;26, Peter Lynch; 27, Gerald Fuller; 28, Serafim Kalliadasis; 29, Anne De Wit; 30, Teresa Stokes; 31, Nicholas Lefebvre; 32, JuliaLong; 33,

26 Mar 2023: surface, either into the atmosphere or under the oceans, travelling along the ground at 24.

25 Mar 2015: occurred more often than two sixes in 24 throws. The mathematicians founded probability theory and showed that the gambler’s instinct was right: one six in four throws is 3% more ... likely to occur than two sixes in 24 throws.

11 Apr 2013: From the exactsolution we have. W0 =. Z2 1 (π2. 24. ... 4.24). This inner solution indeed satisfies the tip condition w0,in = 0 as Z 0, and asZ it reproduces the source term seen in (4.23).

21 Nov 2014: RESEARCH ARTICLE10.1002/2014WR015335. Capillary pinning and blunting of immiscible gravity currents inporous mediaBenzhong Zhao1, Christopher W. MacMinn2, Herbert E. Huppert3,4,5, and Ruben Juanes1. 1Department of Civil and Environmental Engineering,

20 Nov 2014: Accepted article online 24 JUL 2014. Published online 2 SEP 2014. ... FT 5 24=3k. klaT gcl. kl m. 1=3Tl 2TLðClÞ4=3; (16). where aT 5aT TL Clð Þ; Clð Þ is a temperature- and salinity-dependent thermal expansion coefficient calculatedfrom

9 Mar 2004: J. Fluid Mech. (1998), vol. 359, pp. 109–142. Printed in the United Kingdom. c 1998 Cambridge University Press109. Effects of external flow on compositional andparticle gravity currents. By M A R K A. H A L L W O R T H, A N D R E W J. H O G GA N D

5 May 2006: c). 100. 300. 500. 700. = 0.0500. g′ = 19.24 cm s–2.

30 May 2006: J. Fluid Mech. (1996), 001. 308, p p. 289-311 Copyright @ 1996 Cambridge University Press. 289. Entrainment into two-dimensional and axisymmetric turbulent gravity currents. BY M A R K A. H A L L W O R T H ' , H E R B E R T E. H U P P E R T ' , J E

30 May 2006: 0, for which case the third term in (24) is negligible and the single-layer shallow-water momentum equation is recovered. ... The two-layer model comprises the three equations (17), (21) and (24) for the three variables h, u and 4 that describe the

5 May 2006: J. Fluid Mech. (2006), vol. 549, pp. 99–129. c 2006 Cambridge University Pressdoi:10.1017/S0022112005007500 Printed in the United Kingdom. 99. Numerical modelling of convection ina reactive porous medium with a mobile. mush–liquid interface. By

9 Mar 2004: are captured by Figure 4.[24] The calculations in Figure 4 illustrate that volcanic.

25 Jan 2007: J. Fluid Mech. (1989), voZ. 198, p p. 293-319. Printed in Great Britain. 293. Phase changes following the initiation of a hot turbulent flow over a cold solid surface. By HERBERT E. HUPPERT Department of Applied Mathematics and Theoretical Physics,

12 Apr 2013: H = (Q/ub)1/2, (24)and the dimensionless height profile f is solely a function of y, the scaled similarity variable, definedas.

2 Jun 2015: Dashed lines indicate thetheoretical late-time predictions (3.24) and (3.25) for the current radius rf and the widthof the time-dependent frontal region rf rs respectively. ... 3.24). The width of the frontal region at late times can be determined by

9 Feb 2004: 870.0 461.1A25 9 3.0 8.0 24.0 500.0 0.432 1.957 939.0 479.8. ... 675.6 0.350 1.776 761.2 428.A13 53 3.0 8.0 24.0 500.0 0.432 1.957 939.0 479.

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

27 Apr 2006: Once the local Rayleigh number based on 8 exceeds a critical value, as determined by Smith [24] for example, the boundary layer breaks down and the magma begins to convect.

5 May 2006: 14 24.4 8.5 380 015 25.2 17.1 276 016 26.2 34.1 204 017 25.9 63.2 171 018 103.3 8.3 90 019 ... 164 2.913 25.6 33.3 0.123 510 2.930 24.6 16.8 0.123 270 2.931 50 16.8 0.123 240 2.932 104.1

8 Jun 2012: 8 of 21. [24] Thus, disentangling the effects of varying reflectioncoefficient and signal strength is not straightforward, espe-cially when tuning effects are important.

7 Aug 2008: and silt between ice lenses[19,24]. ... Phys. 78, 695 (2006).[24] G. Beskow, The Swedish Geological Society, C, no.

26 Mar 2023: Received: 21 August 2022. Accepted: 11 November 2022. Published: 24 November 2022. ... where 0 < ε << 1 and n 2 is an integer, (24).

1 Jun 2006: Okuz. 24 FLU 251.

19 Jul 2010: Trans. Geotherm.Res. 24 (1985) 25. Roy. Soc. London A310(1984) 511. [19] H.E.

23 Dec 2021: s. h. ttps. ://do. i.org. /10. 1017. /jfm. 201. 7.24. 3. ... term. s. h. ttps. ://do. i.org. /10. 1017. /jfm. 201. 7.24.

20 Nov 2014: Sayag1 and M. Grae Worster1. Received 8 September 2013; revised 24 October 2013; accepted 24 October 2013; published 19 November 2013.

26 Apr 2006: H inner H s0D D0. 1. 1 : (24). Importantly, we have a value for the apparent cotangent.

9 Mar 2004: H.) 3–24 (Springer, Berlin, 1990). 5. Nakada, S., Shimizu, H. & Ohta, K.

30 May 2006: which lead t o the eigenvalue problem? 4" [Jy2(y - c)-2 - $1 $75 = 0) (2.24) = o ( y = T ). ( 2. 2 5 a, b ). There are two infinite families of

23 Dec 2021: In addition,power law fits provide α1 = 0.810.07, β1 = 0.310.02, α2 = 2.50.24,and β2 = 0.140.03.

18 May 2017: 23 DECEMBER 2016. 0031-9007=16=117(26)=268001(5) 268001-1 2016 American Physical Society. the crack, and a Nikon D7100 camera (1920 1080 pixels,frame rate 24 fps) is

9 Apr 2013: a[1 exp(bt)].[24] This exponential time dependence is explained by our. ... Res. Lett., 24(10), 1251–1254. Worster, M. G. (1992), The dynamics of mushy layers, in InteractiveDynamics of Convection and Solidification, NATO ASI Ser.

15 Jul 2010: After 24 hours the fluid at the surface and floor had reached compositions of about 17 wt.% and 25 wt.% NaNO, respectively. ... Volcanol. Geotherm. Res. 24, 25-54, 1985. J.S. Turner, Buoyancy Effects in Fluids, Cambridge Uni- versity Press, Cambridge,

19 Oct 2006: Lett., 24, 1251–1254. Wettlaufer, J. S., M. G. Worster, and H.

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.