Solution

ID: past-exam-of-the-physics-of-atmospheres-and-oceans-course-of-the-university-of-oxford/2019/6/c/solution

For constant , substitution of the vertical cosine and horizontal plane wave gives
The top rigid-lid condition is satisfied by . To select a discrete vertical mode one must also impose the corresponding no-flow, adiabatic condition at the flat bottom, . It requires . The mode is barotropic; the gravest nonzero baroclinic mode has . Hence
The lid condition alone is insufficient: also has zero derivative at the lid but violates the bottom condition. Constant depth motivates the additional physical boundary, which must be used to obtain the printed denominator.
Let and set . The zonal phase velocity and group velocity are
The phase curve is even in , with limiting value at zero and approach to from below at large . The group curve is also even: it starts at the same long-wave limit, equals at , reaches at , and approaches from above at large . The normalized curves appear in the bottom panels of the preceding figure. For , the phase speed means the limit ; there is no zonal crest propagation to define directly at exactly zero wavenumber.

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