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...
שמור ב:
| Autores principales: | , , , |
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| פורמט: | info:eu-repo/semantics/article |
| שפה: | eng |
| יצא לאור: |
Iniversidad Autónoma de Baja California
2013
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| גישה מקוונת: | https://www.cienciasmarinas.com.mx/index.php/cmarinas/article/view/2190 |
| תגים: |
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