In the Northern hemisphere, surface layers are displaced 45° to the right of winds due to the Coriolis effect. The layer below the surface is dragged along by the one above and is displaced a little more than 45°, the layer below that is then dragged along and displaced a little more than 45°, and the effect spirals down until the energy dissipates. This is called: a. Ekman spiral b. Ekman transport c. Ekman layer d. Ekman drift
In the Northern hemisphere, surface layers are displaced 45° to the right of winds due to the Coriolis effect. The layer below the surface is dragged along by the one above and is displaced a little more than 45°, the layer below that is then dragged along and displaced a little more than 45°, and the effect spirals down until the energy dissipates. This is called: a. Ekman spiral b. Ekman transport c. Ekman layer d. Ekman drift
Applications and Investigations in Earth Science (9th Edition)
9th Edition
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Chapter1: The Study Of Minerals
Section: Chapter Questions
Problem 1LR
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In the Northern hemisphere, surface layers are displaced 45° to the right of winds due to the Coriolis effect. The layer below the surface is dragged along by the one above and is displaced a little more than 45°, the layer below that is then dragged along and displaced a little more than 45°, and the effect spirals down until the energy dissipates. This is called:
a. Ekman spiral
b. Ekman transport
c. Ekman layer
d. Ekman drift
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