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Climatological mean and decadal change in surface ocean pCO2, and net seaair CO2 flux over the global oceans
A climatological mean distribution for the surface water pCO2 over the global oceans in non-El Nino conditions has been constructed with spatial resolution of 4° (latitude) ×5° (longitude) for aExpand
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Corrigendum to "Climatological mean and decadal change in surface ocean pCO2, and net sea-air CO2 flux over the global oceans" [Deep Sea Res. II 56 (2009) 554-577]
Taro Takahashi a, , Stewart C. Sutherland , Rik Wanninkhof , Colm Sweeney , Richard A. Feely , David W. Chipman , Burke Hales , Gernot Friederich , Francisco Chavez , Christopher Sabine , AndrewExpand
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The Carbon budget of the North Sea
Abstract. A carbon budget has been established for the North Sea, a shelf sea on the NW European continental shelf. The carbon exchange fluxes with the North Atlantic Ocean dominate the gross carbonExpand
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Rare earth elements in the Pacific and Atlantic Oceans
Abstract The first profiles of Pr, Tb, Ho, Tm and Lu in the Pacific Ocean, as well as profiles of La, Ce, Nd, Sm, Eu, Gd and Yb, are reported. Concentrations of REE (except Ce) in the deep water areExpand
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Synthesis of iron fertilization experiments: From the iron age in the age of enlightenment
Comparison of eight iron experiments shows that maximum Chl a, the maximum DIC removal, and the overall DIC/Fe efficiency all scale inversely with depth of the wind mixed layer (WML) defining theExpand
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Growth rates of large and small Southern Ocean diatoms in relation to availability of iron in natural seawater
Blooms of large diatoms dominate the CO2 drawdown and silicon cycle of the Southern Ocean in both the past and present. The growth of these Antarctic diatoms is limited by availability of iron (andExpand
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Biogeochemical cycling of zinc and its isotopes in the Southern Ocean
Abstract We report Zn concentration and isotope data for seawater samples from the Atlantic sector of the Southern Ocean, collected during the IPY/GEOTRACES ANT-XXIV/III cruise along the GreenwichExpand
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Low dissolved Fe and the absence of diatom blooms in remote Pacific waters of the Southern Ocean
The remote waters of the Pacific region of the Southern Ocean are the furthest away from any upstream and upwind continental Fe sources. This prime area for expecting Fe limitation of the planktonExpand
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Atmospheric iron deposition and sea-surface dissolved iron concentrations in the eastern Atlantic Ocean
Atmospheric iron and underway sea-surface dissolved (<0.2 μm) iron (DFe) concentrations were investigated along a north-south transect in the eastern Atlantic Ocean (27°N/16°W-19°S/5°E). FeExpand
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