New PDF release: 3D ORIGAMI

By Ikuko Mitsuoka

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A theory to remedy this difficulty is advanced in the following section. 4. "Decoup/ed mean" theory The "decoupled mean" theory may seem very familiar to the reader at first glance. Don't most classical papers on stability theory start offwith some arbitrary {1 chosen by the author? J. J, with further (integral) constraints to follow. 3. A class of {1 fields or only The Amplitude of Turbulent Shear Flow 395 one can be found marginally stable at any step in the sequence of constraints relating lJ and £.

Figures 3 and 4 summarize this critique. 05 from the R- T formalism. The oscillating curve on Figure 3 is a zero-average departure from the smooth curve, generated as a Reynolds stress from the marginal OrrSommerfeld eigensolution for that profile. The old and new profiles for {/, found by integrating these two curvatures, are shown in Figure 4. -----r-UNSTABLE 1,000 ... +U

HIDE, R. ( 1983), On the dynamics of rotating fluids and planetary atmospheres: A summary of some recent work, PAGEOPH 121, 365-374. INGERSOLL, A. , BEEBE, R. , CoLLINS, S. , et al. ( 1979), Zonal velocity and texture in the Jovian atmosphere inferred from Voyager images, Nature 280, 773-775. INGERSOLL, A. , BEEBE, R. , MITCHELL, J. , et al. (1981), Interaction ofeddies and mean zonal flow on Jupiter as inferred from Voyager 1 and 2 images, J. Geophys. Res. 86, 8733-8743. INGERSOLL, A. , and CuoNG, P.

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3D ORIGAMI by Ikuko Mitsuoka


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