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10 May 2011: New bifurcations in a partially filled, horizontal, rotating cylinder, A. Aitta, in Propagation in non-equilibrium systems, eds.

25 Nov 2011: Present address: Courant Institute of Mathematical Sciences,New York University, New York, New York 10012, USA.takagi@cims.nyu.edu. ... University Press, Cambridge, 2000).[8] G. B. Whitham, Linear and Nonlinear Waves (Wiley, New York,.

13 Apr 2011: We present a new analogue fluid system thatreproduces the convective behaviour of CO2‐enriched brine.Laboratory experiments and high‐resolution numericalsimulations show that the convective flux scales with theRayleigh number to ... Toanswer these

26 Sep 2011: water is required in many different disciplines. This requirement has been strengthened recently by the emergence of the new subject of double-diffusive convection, which studies the fluid motions driven by ... 4) C. Tanford, “The Hydrophobic Effect”,

21 Oct 2011: Finally in 6 we summarize our new findings and brieflydescribe other possible sources of error in the shallow-water model besides interfacialentrainment. ... Atmos. Environ.13, 1241–1247. Cenedese, C. & Adduce, C. 2010 A new parameterization for

10 Mar 2011: processes and environments. New York, etc., John Wiley andSons. Wettlaufer, J.S.

10 Mar 2011: Downloaded By: [Keating, Shane Richard][New York University] At: 14:40 4 March 2011. ... Subsequently, the spikes establish a new lattice, with a correspondingly larger or smaller.

13 Apr 2011: In Sec. III, the results are presented in three parts.The first part provides an overview of the new types of granularflows of sand that arise by varying the flow rate

21 Oct 2011: HUPPERT2†,R. STEPHEN J. SPARKS3 AND ARMIN FREUNDT4. 1Volcanic Risk Solutions, Massey University, Palmerston North, Private Bag 11222, New Zealand2Department of Applied Mathematics and Theoretical Physics, Institute of Theoretical Geophysics,.

21 Oct 2011: he. )Λ. (3.9). Hence, we obtain the principal new equation that governs the flow of a two-phasebuoyancy-driven current,. ... The two-phase governing equation is analogous to its single-phasecounterpart (Huppert & Woods 1995), with the two-phase effects