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27 Apr 2006: Glaciol., 33, 194–200. Eicken, H., H. R. , .

5 May 2006: Details of our finite-difference numericalcode are presented the Appendix. We used a mesh of 320 horizontal and 200 verticalintervals.

30 May 2006: Y f 5 200 -. 6 a. 250 -. 300 -. Salinity ( % o ). I I I I I I I I 34.2 34.3 3 4 4 34.5 34.6 34.7 ... 200. n E. 300. 350. I I 0.1 OC. FIGURE 8.

5 Jan 2006: 3. 4. 5. 6. 100 200 300 400 500. a(cm). t (min). ... b). 1. 2. 3. 4. 5. 0 50 100 150 200 250 300.

27 Apr 2006: 8 c ) and is graphed in Fig. 5. 200 -. 160 h(m). 120. 8 0 -. 4 0 -. 107. o ,6o 26o 36o r(m). ... t f o r d i s c u s s i o n ). 0 200 400 600 Metres I i I. SCALE. Fig. 9.

1 Jun 2006: J. Fluid Mech. (1991), vol. 224, p p. 335-359 Printed i n Great Britain. 335. Natural convection in a mushy layer. By M. G R A E WORSTER Department of Engineering Sciences & Applied Mathematics and Department of Chemical. Engineering, Northwestern

26 Apr 2006: AR266-FL38-16 ARI 22 November 2005 19:29. Premelting DynamicsJ.S. Wettlaufer1 and M. Grae Worster21 Department of Geology and Geophysics, Department of Physics, Yale University, New Haven,Connecticut 06520-8109; email: john.wettlaufer@yale.edu2

5 May 2006: 1. (a). (b). 0 50 100 150 200 250 300 350100.

30 May 2006: 200. n 150 W. 50. 1 I I I I 0 20 40 60 80. ... R. Lister. 60 I n g'. (cm s-3 Expt Theory 42 21 11 0 - -. 0 - A. 0. I - - - 9 - - - --.__ I 100 I 150 I 200.

27 Apr 2006: Fig. 1. The velocity of the head is approximately constant for a distance of about 200 cm, which is approximately ten times the lock. ... 3. Over the first 1.5 m the three. 500. ' 200.