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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. -
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. -
Journal of Fluid Mechanics 251: REVIEWS
www.itg.cam.ac.uk/people/grae/20.pdf1 Jun 2006: Okuz. 24 FLU 251. -
PRL 95, 176102 (2005) P H Y S I ...
www.itg.cam.ac.uk/people/grae/65.pdf26 Apr 2006: H inner H s0D D0. 1. 1 : (24). Importantly, we have a value for the apparent cotangent. -
On Howards technique for perturbing neutral solutions of the…
www.itg.cam.ac.uk/people/heh/Paper14.pdf30 May 2006: which lead t o the eigenvalue problem? 4" [Jy2(y - c)-2 - $1 $75 = 0) (2.24) = o ( y = T ). ( 2. 2 5 a, b ). There are two infinite families of -
gl026290 1..4
www.itg.cam.ac.uk/people/grae/75.pdf19 Oct 2006: Lett., 24, 1251–1254. Wettlaufer, J. S., M. G. Worster, and H. -
Lee waves in a stratified flow Part 3. Semi-elliptical obstacle
www.itg.cam.ac.uk/people/heh/Paper8.pdf30 May 2006: a$'(@, 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-. -
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. -
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 -
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. -
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. -
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. -
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. -
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. -
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. -
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)—. -
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 -
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)—.
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