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30 Jul 2013: 1.0. s. P. n10n4n2. Β=100. Β=5. 1 2 5 10 20 50 1000.10. ... 1.00. 0.50. 0.20. 0.30. 0.15. 0.70. Β. P. 0. n10n4n2. (a) (b).

12 Apr 2013: Received 13 July 2012; accepted 20 December 2012; published online 21 March 2013). ... η = (ϕ2/Qub)1/4 r t 1/2, (20)such that the radius of the current is given by.

11 Apr 2013: 102. 1020 5 10 15 20. FIGURE 3. (a) Fibre tip deflection, u(hy), versus flow rate, Q, for d = 56 µm, D = 66 µm,H = 400 µm and varying values ... The fibres are imaged at a magnification of 20 (see theinset of figure 2) with the same microscope used

11 Apr 2013: 20. 40. 60. 80. 100. 120. 1 2 3 4 5 6 7. ... E. Huppert, J. A. Neufeld and C. Strandkvist. 0 20 40 60 80 100.

14 Feb 2013: 11:. 12:. 13:. 14:. 15:. 16:. 17:. 18:. 19:. 20:. 21:.

11 Apr 2013: a) (b). buoyant fluid ambient fluid. 56 cm. 2, 5, 10or 20 cm. ... 0 5 10 15 20 250. 0.2. 0.4. 0.6. 0.8. 1.

12 Apr 2013: Mixing of an interflow into the ambient water of Lake Iseo. Charlie A. R. Hogg,a, Clelia L. Marti,b Herbert E. Huppert,a,c and Jörg Imberger b. a Institute of Theoretical Geophysics, Department of Applied Mathematics and Theoretical Physics,

14 Feb 2013: 4.1. Buoyant Spreading Without ConvectiveDissolution. [20] In the absence of convective dissolution, the modelfor the spreading of a buoyant current in a confined porouslayer can be written [e.g., Bear, ... 2011]. [45] For an aquifer of thickness H 20 m,

11 Apr 2013: is.about.20.in.the.polar.oceans,.which.is.why.the.densest.abys-sal.waters.are.generated.around.Antarctica,.where.polynyas.are.commonly.formed.by.strong.katabatic.winds.off.the.continent,. ... measure.the. brine. diffusivity. and. volume. fraction. of. ice