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www.damtp.cam.ac.uk/user/phh/atmosocean/atmos-ocean.pdf19 Sep 2005: is. ω2 = f2 gHk2, i.e. ω = (f2 gHk2)1/2. (3.20). The two branches of the dispersion relation correspond to waves with phase propagationin two different directions. ... ithou. t per. mis. sion. P.H.Haynes Mathematics III Atmosphere-Ocean Dynamics -
Part II Statistical Mechanics, Lent 2005 Prof. R.R. Horgan ...
www.damtp.cam.ac.uk/user/rrh/notes/sphys.pdf14 Feb 2005: 2 THERMODYNAMICS 20. where CV is the heat capacity at constant volume and CP is heat capacity atconstant pressure. -
Lucidity, science, and the arts: what we can learn ...
www.damtp.cam.ac.uk/user/mem/kobe-lecture.pdf28 Apr 2005: Notice that the typical period of asingle one of the oscillations is of the order of 200 years, that is, 10 humangenerations if we assume that a generation takes 20 years. ... It is an aspect of hypercredulity. 20. Lacking, at first, the most highly
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