CO<sub>2</sub> maximum in the oxygen minimum zone (OMZ)
Oxygen minimum zones (OMZs), known as suboxic layers which are mainly localized in the Eastern Boundary Upwelling Systems, have been expanding since the 20th "high CO<sub>2</sub>" century, probably due to global warming. OMZs are also known to significantly contribute to the oceanic production of N<...
Uloženo v:
| Hlavní autoři: | , , |
|---|---|
| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
Copernicus Publications
2011-02-01
|
| Edice: | Biogeosciences |
| On-line přístup: | http://www.biogeosciences.net/8/239/2011/bg-8-239-2011.pdf |
| Tagy: |
Žádné tagy, Buďte první, kdo vytvoří štítek k tomuto záznamu!
|