Introductory Dynamical Oceanography¶
Pond, S., & Pickard, G. L. (1983). Introductory Dynamical Oceanography. Pergamon Press.
Cited by¶
1 citation across 1 artifact.
Each citation links to the sentence it supports in the citing article.
Domain-specific¶
- Upwelling
- Persistent winds blowing roughly parallel to a coastline exert a stress on the surface ocean; on a rotating Earth, the Coriolis force deflects the resulting surface current 90° to the right of the wind in the Northern Hemisphere (90° to the left in the Southern), producing a net offshore Ekman transport in a surface layer roughly 50–200 m thick
This sourcePond and Pickard's dynamical-oceanography treatment of wind-driven Ekman flow, in which the surface current runs about 45° to the right (left) of the wind in the Northern (Southern) Hemisphere.
Supported in partVerified against the work's full text
“right of V,, in the [northern] [hemisphere], to the left in the southern [hemisphere].”
- Persistent winds blowing roughly parallel to a coastline exert a stress on the surface ocean; on a rotating Earth, the Coriolis force deflects the resulting surface current 90° to the right of the wind in the Northern Hemisphere (90° to the left in the Southern), producing a net offshore Ekman transport in a surface layer roughly 50–200 m thick
Verification¶
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Registry ID ref:5a89b69be363 · see in the full table