The Gulf of California is a source of carbon dioxide to the atmosphere

Water exchange between the Gulf of California and the Pacific Ocean has a significant vertical component (VCWE). Surface (0–200 m) gulf water flows out into the Pacific Ocean and deep (200–600 m) water flows into the gulf. This is a mechanism that allows for the net input to the gulf of dissolved co...

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Bibliografische gegevens
Hoofdauteurs: Rodríguez-Ibáñez, Claudia, Álvarez-Borrego, Saúl, Marinone, SG, Lara-Lara, José Rubén
Formaat: info:eu-repo/semantics/article
Taal:eng
Gepubliceerd in: Iniversidad Autónoma de Baja California 2013
Online toegang:https://www.cienciasmarinas.com.mx/index.php/cmarinas/article/view/2190
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