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Thursday Seminars on Theoretical Geophysics
www.itg.cam.ac.uk/seminars/thu_2.05/mich_2008.html8 Oct 2008: 13 November. Peter Liss. (UEA). Air-sea exchange of trace gases. 20 November. -
Experimental Verification of Morphological Instabilityin Freezing…
www.itg.cam.ac.uk/people/grae/83.pdf7 Aug 2008: a) Measurements of the osmotic pressure of bentoniteas a function of particle volume fraction (4 [20]; [26]; [27]; [28]). ... Soil Sci. 41, 547 (1990).[20] P. F. Low, D. M. Anderson, and P. -
Ice.dvi
www.itg.cam.ac.uk/people/grae/80.pdf1 Feb 2008: The ratio of these buoyancyfluxes. BF /BC = βS0cp/αL 10 20 (12). ... 10 12 14 16 18 200. 5. 10. 15. 20. 12.9 12.95 13 13.050. -
flm021.dvi
www.itg.cam.ac.uk/people/heh/Paper209.pdf14 May 2008: S. L. Peppin, H. E. Huppert and M. G. Worster. 0 5 10 15 20. ... JOM-J. Min. Met. Mat. Soc. 49, 18–20. Huppert, H. E. 1990 The fluid mechanics of solidification. -
jc004333 1..7
www.itg.cam.ac.uk/people/grae/82.pdf7 Aug 2008: The measurements were carried out with very high vertical and temporalresolution over the course of a few days until the ice had reached a thickness ofaround 20 cm. ... 2002], indicating thatequation (3) might also be a good approximation for theaverage -
Viscous gravity currents inside confining channels and…
www.itg.cam.ac.uk/people/heh/Paper210.pdf5 Mar 2008: 023104-2 D. Takagi and H. E. Huppert Phys. Fluids 20, 023104 2008. ... 023104-4 D. Takagi and H. E. Huppert Phys. Fluids 20, 023104 2008. -
doi:10.1016/j.jcrysgro.2008.04.046
www.itg.cam.ac.uk/people/grae/85.pdf7 Aug 2008: 02ðhÞz. þ zLsVfEke. z zLsVfE2keh. z2, (20). where we evaluate f 01ðhÞ and f02ðhÞ using the assumption h5L, such. -
doi:10.1016/j.jcrysgro.2008.04.046
www.itg.cam.ac.uk/people/heh/Paper212.pdf7 Aug 2008: 02ðhÞz. þ zLsVfEke. z zLsVfE2keh. z2, (20). where we evaluate f 01ðhÞ and f02ðhÞ using the assumption h5L, such. -
Gravity currents from a line source in an ambient flow
www.itg.cam.ac.uk/people/heh/Paper211.pdf7 Aug 2008: 3. –60 –50 –40 –30 –20 –10 0. Figure 3. Location of the different solution structures in (a) (β, D) parameter space withM = U = 0, (b) (β, U) space with M = ... ii),(iii). (i). (i) (iv) (ii). (vi). (v). (ii)(iv). (vi)(v). (iii). –20 –10
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