By R. Craig (Auth.)
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Additional resources for Marine Physics
Ekman in the early years of the century. The ideas give a useful introduction to the problem, and an elegant concept of the way the wind and water stresses must balance each other. The assumption that the viscosity is independent of height and depth is clearly not an accurate one, and it is right also to be highly suspicious of the variations of the various quantities with latitude, at least in the way they have been developed here. It is instructive to look again at some of our formal conclusions to see which are likely to have absolute validity irrespective of the assumptions made heretofore.
Since the momentum rule is absolute, for steady state conditions, the stress can make no difference to the total momentum generated by F. Instead, the stress acts by generating equal and opposite supplementary momenta in the air and water. It will be recalled that the velocity spiral in the air (or in the water) is such that in some small increment δ of height the vector of induced velocity decreases as e~qd and the direction of the vector changes by an angle qd 3. WIND CURRENTS IN DEEP WATER 35 radians.
Thus 4. QUALITATIVE PHYSICAL OCEANOGRAPHY 39 the situation is by no means simple and the effect of wind driven transport is to combine with other effects in progressively destroying the discontinuity which, formed during the early summer, is continually being "nibbled away" at the edges (Fig. 4b). c ► -*— ^— J) (a) Fig. 4. Wind-driven currents in the prescence of a thermocline. Since this is a practical chapter, gathering together ideas, it may be permissible to complete this statement by showing, in Fig.
Marine Physics by R. Craig (Auth.)