Abstract
This paper analyses a western boundary current striking a solid boundary. Interest is concentrated on the case where inertial effects are sufficient to modify the flow from its 'Stommel-layer' form with Ekman friction relatively unimportant in the interior. It is shown that, beyond a critical inflow speed, a complicated system of four asymptotic regions forms near the corner, turning some of the flow along the blocking boundary and then returning it westwards to rejoin the western boundary current. A comparison with the results of a simple ocean model shows that many of the features in that flow can be explained through the asymptotic theory.
Original language | English |
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Pages (from-to) | 477-504 |
Number of pages | 28 |
Journal | Dynamics of Atmospheres and Oceans |
Volume | 15 |
Issue number | 6 |
DOIs | |
Publication status | Published - 1 Jan 1991 |