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5 Oct 2009: 20 October. Sue Liu. (DAMTP). Transport and dehydration in the tropical tropopause layer.

14 Sep 2009: Style1 and M. Grae Worster1. Received 22 January 2009; revised 20 April 2009; accepted 6 May 2009; published 10 June 2009.

20 Jan 2009: Last modified: 20 January 2009 by dia. Comments & suggestions, email.

4 Jun 2009: 1030. 25. 20. 5. 8. 6. 4. 2. 0. –20 0.5 1.0 1.5. ... plotted for times T = 5 (solid line), 10 (dotted line), 15 (short-dashed line), 20(dash–dotted line), 25 (long-dashed line) and 30 (dashed–dotted–dotted line).

18 Nov 2009: 10. 20. 30. 40. 50. 60. y. 0 5 10 15 20 25 30 35 400. ... Fluids 20 (2008) 1–8 023104. [21] M.I. Cantero, J.R. Lee, S.

24 Sep 2009: 1.0. 1.5. 2.0. 20 40 60 80 100 120 1400. 1. ... 1. 2. 3. 4. 10 20 30 40 50 60 70 80 90.

14 Sep 2009: 2 gives an extreme counterexample to the applicability ofthe model for the simulation of sea ice.[20] As an aside, Figure 2 also shows the solid fraction field. ... perature gradient of 10C/m, a brine diffusivity of D 6.8 1010 m2 s1, a brine salinity of

18 Nov 2009: χ 1 ζ /ζ0, (3.10)and letting. ϕ(χ) H 0 /ζ 20. ... 5 10 15 20 25 30 350. 0.2. 0.4. 0.6. 0.8.

14 Sep 2009: 0. -10. -20. A schematic phase diagram of the binary NH4 Cl–water system. ... 6. Note that the mushy layer is laterally uniform for more than 20 min before theinstability occurs.

10 Mar 2009: Consequently, Kc(0) = 0 and, using (2.1)–(2.4), we obtain. Pc(0) =. (1. 4ρor. 20 h. 20g. ′) [. 1 S 13. S. ... 20 h. 20g. ′ and ηwith h0. As expected, the energy terms for the current are similar to these derived for theSW case.