## Abstract A synopsis is offered of circulation mechanisms in the oceanic regions of the equatorial zone. Over the eastern Atlantic and Pacific, and especially in boreal summer, crossβequatorial flow from the Southern Hemisphere is strong and induces a tongue of cold surface waters, centred to the
Dynamics of the Pacific Equatorial Dry Zone
β Scribed by S. Hastenrath
- Publisher
- Springer
- Year
- 1999
- Tongue
- English
- Weight
- 469 KB
- Volume
- 71
- Category
- Article
- ISSN
- 1436-5065
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