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5 Jan 2006: The experimentswere generally left to run for 24 hours, but heat loss to the laboratory became asignificant factor after roughly 10 hours. ... dy. dτ= (1 θ). (1 y)(1 Λθ). (3.24). y(τ = 0) = 1, (3.25).

24 Jan 2006: Please bring your own lunch. 24 January. Thibaut Putelat. (ITG). On the selection of active fault planes.

26 Apr 2006: H inner H s0D D0. 1. 1 : (24). Importantly, we have a value for the apparent cotangent.

26 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.

26 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.

26 Apr 2006: Leppäranta, pp. 24–104,Univ. of Helsinki Press, Helsinki, 1998. Wettlaufer, J. S., Heat flux at the ice-ocean interface, J. ... E. Huppert, The phase evolution ofyoung sea ice, Geophys. Res. Lett., 24, 1251–1254, 1997a.

26 Apr 2006: Received 29 March 2004; received in revised form 24 September 2004; accepted 11 November 2004. ... ykumar and Mao [24] again assuming the interface was sharp. The SPH method, as mentioned earlier, does.

26 Apr 2006: 1.0 [24]. The slope of the linethrough data set (h), for silicon carbide particles in a succino-nitrile melt, is! ... Azouni, W. Kalita, M. Yemmou, J. Crystal Growth. 99 (1990) 201.[24] S.

26 Apr 2006: Using equations (3) and (22)–(24), it is possibleto calculate _h, S0 and T0 in terms of far-field properties T1and S1 by eliminating two of the unknowns to obtain aquadratic ... For this simula-tion we used again the values given in Table 1 and Si =

26 Apr 2006: salinity of the ice) is very small; k #1 0 24 [Gross et al., 1987].