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Mesoscale variable internal

The second example is the case in which the disperse-phase velocity is equal to the conditional expected disperse-phase velocity given the other mesoscale variables Vp = (Upl p, Vf, f). In this case, fluctuations in the disperse phase are slaved to the fluid-phase fluctuations and can depend on the particle internal coordinates (e.g. particle size). The NDF in this case is n(Vp, p, Vf, f) = n( p, Vf, f)(5(Vp - [Pg.131]

Eremeev VN, Ivanov VA, Kosarev AN, Tuzhilkin VS (1992) Climatic thermohaline fields of the Black Sea waters with mesoscale resolution three-dimensional structure and annual variability. In Problems of the Black Sea (international conference). Sebastopol, Ukraine, 10-15 November 1992. MHI UAS, Sebastopol, p 209... [Pg.252]

See other pages where Mesoscale variable internal is mentioned: [Pg.23]    [Pg.17]    [Pg.19]    [Pg.112]    [Pg.148]    [Pg.149]    [Pg.160]    [Pg.545]    [Pg.545]    [Pg.134]    [Pg.115]    [Pg.163]    [Pg.109]    [Pg.137]    [Pg.153]    [Pg.173]   
See also in sourсe #XX -- [ Pg.19 ]



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Internal variables

Mesoscale

Mesoscale variability

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