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This paper studies the vibration characteristics of a rotating tapered cantilever Bernoulli Euler beam with linearly varying rectangular cross-section of area proportional to xn, where n equals to 1 or 2 covers the most practical cases.
Figure 4 Time-height cross sections of area-mean θ ′ w ′ ¯ (upper panels) and q ′ w ′ ¯ (lower panels).
Figure 4 shows time-height cross sections of area-mean θ ′ w ′ ¯ and q ′ w ′ ¯ in cases A02 to A20.
Figure 9 shows time-height cross sections of area-mean u ′ w ′ ¯ for UZ values of 0 and 3 m · s 1 · km 1.
Time-height cross sections of area-mean θ ′ w ′ ¯ for cases B1, B3, and B5 are shown in the upper panels of Figure 8.
Figure 13 Time-height cross sections of area-mean θ ′ w ′ ¯ (left panels), q ′ w ′ ¯ (middle panels), and u ′ w ′ ¯ (right panels).
Figure 5 Time-height cross sections of area-mean u ′ w ′ ¯ in U Z = 0 and 3 (m · s -1 · km -1 ; upper and lower panels, respectively).
The eddy momentum flux is sensitive to the initial vertical shear of zonal flow UZ. Figure 5 shows time-height cross sections of area-mean u ′ w ′ ¯ for UZ values 0 and 3 m · s-1 · km-1.
Thin sections of areas containing midgut were stained with uranyl acetate and lead citrate, and examined in a Hitachi H7650.
A mesotrophic lake lay in the areas near the sea, while a eutrophic lake was located in the middle section of the area.
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