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6 May 2010: where representative valuesof ρ = 1.4 kg m3, g = 9.8 m s2, γ = 78 mN m1 and R = 0.24 m were fixed. ... and R = 0.24 m. Wavelengths were estimated by dividing the circumference of the leading edgeof the flow at the onset of instability by the number of

5 May 2006: 24 48.2 20.9 26 120 0.83 2.6 1760 2.7 1.38 48.2 20.5 20.3 20 1.18 1.5 2250 2.1 ... 34. 32. 30. 28. 26. 24. 22. 20. 18. 16. 14.

13 Nov 2007: Method. Glass beads 24 Rotating drume. 0.25–0.35 24 Smooth inclined planef. ... 0.5 0.04 24–31 Rough inclined planeg. 1.26 9–11 Shear gauge, smooth chute flowh.

19 Jul 2010: η1. )w2(0),. (24). (. 1. k2D3 D. )w1(0) η2. η1. (1.

12 Apr 2013: Parameter Value. Inflow channel width (m) 49Inflow channel depth (m) 1.7Inflow velocity (m s21) 0.48Inflow reduced gravity (m s22) 0.021Inflow temperature (uC) 13.0Lake surface temperature (uC)

5 May 2006: www.damtp.cam.ac.uk/lab/digiflow/ 2005.23 G. S. Campbell, Annu. Rev. Fluid Mech. 22, 57 1990.24 T.

9 Apr 2013: These colloidal concentration gradients, which areneglected in rigid-ice formulations, can trigger a thermody-namic instability that leads to morphological transitions in thepattern of segregated ice.23,24 Recently, these thermodynamicprinciples

1 Jun 2006: E. Huppert. Parameter Value Units. a (5.0+ 0.24( T- 20)) x U 0.015 cm2 s-' CC 4.14 J O C - '. 2.66 J cm-3 O C - '

9 Feb 2004: The volume fration of particles in suspension evolves as23,24. df. dt5. ... X5 x/l , 24! T5 t/ v sl /q!1/ a 2 1!, 25!

9 Mar 2004: 15 P 24.2 P25.2 L25.2 P25.2 P30.2 L. T (C) T (C).

14 Sep 2009: is in the direction of rT).[24] Typical advection velocities estimated from a tem-. ... Assur, A. (1958), Composition of sea ice and its tensile strength, in ArcticSea Ice; Conference Held at Easton, Maryland, February 24–27, 1958,pp.

27 Apr 2006: Subsequently (ap- proximately 40-50 rain from the beginning),. 24 r. KOYa_GUCHI L, kt. ... grade particles with A T = 2 4 C and Co= 1.24 wt.%.

12 Mar 2004: requires. P q02pd. : 24. Equation (24) thus links the dendrite tip radius to. ... This solution has a scaled tip radius P = 10.8. and a scaled tip position Z 2:24.

10 Jun 2004: a. r – riri. sandsaltricecouscoussugar slope 1.24. Figure 9. The non-dimensional radial excursion, (r ri )/ri , as a function of the aspect ratioa with a < 1.7 for sand, salt, ... A straight line through the origin atslope 1.24 has a regression

21 Mar 2016: Assessment of ice flow dynamics in the zone close to the calvingfront of Antarctic ice shelves. Martin G. WEARING,1;2 Richard C.A. HINDMARSH,1 M. Grae WORSTER2. 1British Antarctic Survey, Natural Environment Research Council, Cambridge,

9 Apr 2013: 2 2 2. 24/.467. 35.1 Introduction.

9 Mar 2004: Indeed, for most of the experimentsdiscussed by TML λ was in the range 0.02–0.24. ... tr dr rN. drNdthN. (2.24). We eliminate h/t with the aid of (2.12) and, after some rearrangement, we againobtain the result (2.22).

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

21 Oct 2011: The camera was operated at 1000 frames s1. and a resolution of 640 512 pixels (24 bits). ... 18.8 cm. 24.7 cm. 31.1 cm. 37.6 cm. 43.3 cm. 49.7 cm.

25 Jan 2007: E. Huppert. Parameter Value Units. a (5.0+ 0.24( T- 20)) x U 0.015 cm2 s-' CC 4.14 J O C - '. 2.66 J cm-3 O C - '