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Convection and particle entrainment driven by differential…
www.itg.cam.ac.uk/people/heh/Paper99.pdf30 May 2006: t would have the same settling velocity in water a t 20 "C. ... 0655. R 0.01 0.14 0.22 0.28 0.44 0.63 0.84. 0 5 10 15 20. -
PII: 0012-821X(90)90126-I
www.itg.cam.ac.uk/people/heh/Paper98.pdf27 Apr 2006: b Institute of Theoretical Geophysics, University of Cambridge, 20 Silver Street, Cambridge CB3 9EW, U.K. " ... 100. 8O. 60. 40. 20. O " '. ". ' ". " ' -. 0 50 100 150 200. TIME (yrs) Fig. -
PII: 0012-821X(90)90143-L
www.itg.cam.ac.uk/people/heh/Paper97.pdf27 Apr 2006: N. W i l s o n a. a Department of Geology, Wills Memorial Building, Bristol University, Bristol BS8 1RJ (U.K.) b Institute of Theoretical Geophysics, 20 Silver Street, University -
Lee waves in a stratified flow. Part 4. Perturbation approximations
www.itg.cam.ac.uk/people/heh/Paper9.pdf30 May 2006: 00. c, = - K / {2(:(2)Kg2(2))r’(x)dx. (5.20) - 0 0. ... Calculating L(x) through 0(tc2) and aub- stituting the result into (5.20), we obtain. -
PII: 0012-821X(89)90063-0
www.itg.cam.ac.uk/people/heh/Paper87.pdf27 Apr 2006: 0(1 - 1.67x)-2"5, (20). where #0 -- 30 P a s is the viscosity a t 1200 C a n d x is the f r a c t -
The Generation of Granitic Magmas by Intrusion of Basalt ...
www.itg.cam.ac.uk/people/heh/Paper83.pdf15 Sep 2006: 2 Department of Earth Sciences, Downing Street, Cambridge CB2 3EQ. (Received 20 July 1987; revised typescript accepted 14 January 1988). ... This temperature profile is governed by the diffusion equation. 36 326— = , —y (20). -
The stability of a large gas bubble rising through liquid
www.itg.cam.ac.uk/people/heh/Paper81.pdf30 May 2006: 20. 16. 8. J. 0.2 0.4 0.6 0.8. 0.082 uo/[ (cm/s). -
Lee waves in a stratified flow Part 3. Semi-elliptical obstacle
www.itg.cam.ac.uk/people/heh/Paper8.pdf30 May 2006: BLANCH, G. 1964 Mathieu Functions, chapter 20 in Handbook of Mathematical Functions (edited by M. -
PII: 0377-0273(82)90062-2
www.itg.cam.ac.uk/people/heh/Paper48.pdf27 Apr 2006: 204. ,0 l 0.8 0 6 t=lO 2. o ,'o 20 30 4'o s'o r (crn). -
The propagation of two-dimensional and axisymmetric viscous gravity…
www.itg.cam.ac.uk/people/heh/Paper47.pdf30 May 2006: Substituting (2.19) into (2.20), we obtain. to which must be added the global continuity equation. ... 5 = (fg1Q3/V)-Brt-(3i1)/8 and. h(r> t , = @“(3&V/g’)a $([/EN),. (2.20).
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