Towards accounting for dissolved iron speciation in global ocean models
The trace metal iron (Fe) is now routinely included in state-of-the-art ocean general circulation and biogeochemistry models (OGCBMs) because of its key role as a limiting nutrient in regions of the world ocean important for carbon cycling and air-sea CO<sub>2</sub> excha...
| Main Authors: | , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2011-10-01
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| Series: | Biogeosciences |
| Online Access: | http://www.biogeosciences.net/8/3025/2011/bg-8-3025-2011.pdf |