Unidad Océano y Clima, Instituto de Oceanografía y Cambio
Global, IOCAG, Universidad de Las Palmas de Gran Canaria, ULPGC, Unidad
Asociada ULPGC-CSIC, Canary Islands, Spain
Unidad Océano y Clima, Instituto de Oceanografía y Cambio
Global, IOCAG, Universidad de Las Palmas de Gran Canaria, ULPGC, Unidad
Asociada ULPGC-CSIC, Canary Islands, Spain
Daniel Santana-Toscano
Unidad Océano y Clima, Instituto de Oceanografía y Cambio
Global, IOCAG, Universidad de Las Palmas de Gran Canaria, ULPGC, Unidad
Asociada ULPGC-CSIC, Canary Islands, Spain
Unidad Océano y Clima, Instituto de Oceanografía y Cambio
Global, IOCAG, Universidad de Las Palmas de Gran Canaria, ULPGC, Unidad
Asociada ULPGC-CSIC, Canary Islands, Spain
Unidad Océano y Clima, Instituto de Oceanografía y Cambio
Global, IOCAG, Universidad de Las Palmas de Gran Canaria, ULPGC, Unidad
Asociada ULPGC-CSIC, Canary Islands, Spain
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Total article views: 908 (including HTML, PDF, and XML)
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710
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Total article views: 1,284 (including HTML, PDF, and XML)
Thereof 1,234 with geography defined
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Total article views: 908 (including HTML, PDF, and XML)
Thereof 868 with geography defined
and 40 with unknown origin.
Total article views: 376 (including HTML, PDF, and XML)
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The pathways of the Atlantic circulation form a complex system of currents that change meridionally due to interactions with nearby water masses. Over the last 30 years, hydrographic data have allowed us to characterize these upper, deep, and abyssal currents for the entire water column using high-resolution data, computing their mass, heat, and freshwater transports. Generally, we have found no changes among decades for each current in terms of the transport of mass or properties.
The pathways of the Atlantic circulation form a complex system of currents that change...