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This case is similar to what is often called "geostrophic flow," in which Coriolis and pressure forces balance each other in a steady (time-independent) way.
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This case is similar to what is often called "geostrophic flow," in which Coriolis and pressure forces balance each other in a steady (time-independent) way.
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Though our device is a spherical shell, its modes are well approximated by the full-sphere modes, consistent with expectations from theoretical work; in fact, some full-sphere modes persist unchanged in a spherical shell. The change in geometry does have consequences, however, as will be discussed further below.
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Though our device is a spherical shell, its modes are well approximated by the full-sphere modes, consistent with expectations from theoretical work; in fact, some full-sphere modes persist unchanged in a spherical shell. The change in geometry does have consequences, however, as will be discussed further below.
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