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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. -
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 -
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-. -
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. -
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.
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