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17 Jan 2011: 24 February. MR9. Thierry Alboussiere. (ENS Lyon). The 'not so quiet' inner core.

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

21 Dec 2012: Carbon budgets have been introduced to capemissions [24] (Figure 1). The power sector is the single largest emitter. ... and are designed to capemissions [24] (green line).

5 May 2006: We areinterested in cases with small C2H because otherwise the distance of propagation issmall, see (3.24), and no real gravity current appears. ... Using the approximations (3.19)–(3.24), we find: (i) for S < 1.

10 Mar 2009: Conservation of volume. v = 0. (2.24)2. Momentum balance. ρDv. Dt= p (ρ ρb)g ẑ μ2v, (2.25). ... After some algebra and use of(2.24), we obtain. ρD. Dt. [1.

9 Feb 2004: 5H1 2(H0U1)′=0, (24)3U1 H ′1 H ′0ϕ1. 1. 2H0ϕ. ′1=0, (25)ϕ1=2720. ... 4y2)], (38). and then subsequent substitution into (24) yields a second-order differential equation forH1(y), namely(1.

23 Dec 2021: 2πϕ r0. 0. h00. s0[h0(r), z]dzr dr =V, (2.24). where s0[h0(r), z] is the initial saturation distribution. ... By applying scaling analysis to (2.14) and (2.24) and rearranging, we find thefollowing relations between the dimensions of radius, height,

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 - '

24 Apr 2014: The approximate constancy of the late-time first-ordercorrection (E 1.38t1/2) 0.24 is due to the adjustment of the radial flow near thesource towards unidirectional flow over a

9 Mar 2004: Consequently, the relationships between the variables on the characteristics with. 24 M. ... v = r[1. (rinitr. )2]. (2.24). In particular, at the nose.