Fluxes and distribution of dissolved iron in the eastern (sub-) tropical North Atlantic Ocean

Aeolian dust transport from the Saharan/Sahel desert regions is considered the dominant external input of iron (Fe) to the surface waters of the eastern (sub‐) tropical North Atlantic Ocean. To test this hypothesis, we investigated the sources of dissolved Fe (DFe) and quantified DFe fluxes to the s...

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Veröffentlicht in:Global biogeochemical cycles 2012-09, Vol.26 (3), p.n/a
Hauptverfasser: Rijkenberg, Micha J. A., Steigenberger, Sebastian, Powell, Claire F., van Haren, Hans, Patey, Matthew D., Baker, Alex R., Achterberg, Eric P.
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Sprache:eng
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