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Depth profile of Fe solubility from GO-Flo station M68/3_258
DFG grant CR145/5-1 (contribution to German SOLAS). WOCE quality flags converted to internal format, see hdl:10013/epic.31518.d001 -
Depth profile of Fe solubility from GO-Flo station M68/3_307
DFG grant CR145/5-1 (contribution to German SOLAS). WOCE quality flags converted to internal format, see hdl:10013/epic.31518.d001 -
Nitrogen and carbon fixation rates during METEOR cruise M90
This dataset has no description
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Modeled uncertainties in marine N2O emissions with links to source files (52 ...
The ocean is responsible for up to a third of total global nitrous oxide (N2O) emissions, but uncertainties in emission rates of this potent greenhouse gas are high (>100%).... -
Particle characterization at CVAO during the 2008 Intensive III
Mass: Mettler-Toledo UMT2 after 48 h equilibration of the impactor foils at 20 °C and 50 % rel. humidity.IC: Parts of the impactor foils (about 30 %) were extracted by the... -
Long-term chemical characterization of aerosols at CVAO from 2007 to 2011
The first long-term aerosol sampling and chemical characterization results from measurements at the Cape Verde Atmospheric Observatory (CVAO) on the island of São Vicente are... -
Long-term chemical characterization of aerosols at CVAO from 2012 to 2013
The sampling regime has been changed several times. All changes are described by Fomba et al. (2014). The PM10 filter were stored in a freezer at Mindelo and transported frozen... -
Hydrochemistry during ISLANDIA cruise ISL_00311
CVOO: Cape Verde Ocean Observatory Project -
Particle characterization at CVAO during the 2012 Intensive VIII
Mass: Mettler-Toledo UMT2 after 48 h equilibration of the impactor foils at 20 °C and 50 % rel. humidity.IC: Parts of the impactor foils (about 30 %) were extracted by the... -
Particle characterization at CVAO during the 2009 Intensive IV
Mass: Mettler-Toledo UMT2 after 48 h equilibration of the impactor foils at 20 °C and 50 % rel. humidity.IC: Parts of the impactor foils (about 30 %) were extracted by the... -
Particle characterization at CVAO during the 2010 Intensive V
Mass: Mettler-Toledo UMT2 after 48 h equilibration of the impactor foils at 20 °C and 50 % rel. humidity.IC: Parts of the impactor foils (about 30 %) were extracted by the... -
Particle characterization at CVAO during the 2011 Intensive VII
Mass: Mettler-Toledo UMT2 after 48 h equilibration of the impactor foils at 20 °C and 50 % rel. humidity.IC: Parts of the impactor foils (about 30 %) were extracted by the... -
Particle characterization at CVAO during the 2010 Intensive VI
Mass: Mettler-Toledo UMT2 after 48 h equilibration of the impactor foils at 20 °C and 50 % rel. humidity.IC: Parts of the impactor foils (about 30 %) were extracted by the... -
Particle characterization at CVAO during the 2013 Intensive IX
Mass: No mass available for the whole campaign.IC: Parts of the impactor foils (about 30 %) were extracted by the identical method in 1.5 ml high purity water (>18.1 ohm cm).... -
Iron analysis in bottle profiles off Mauritania
Iron solubility measurements in the Mauritanian upwelling and the adjacent Open Ocean of the Tropical Atlantic show for all stations lower values in the surface mixed layer than... -
Noble gases sampled from three cruises in the eastern tropical Atlantic in Se...
Upwelling velocities w in the equatorial band are too small to be directly observed. Here, we apply a recently proposed indirect method, using the observed helium isotope (3He... -
Gel particles in the sea-surface microlayer during an experimental study
Since the early 80's, the sea-surface microlayer (SML) has been hypothesized as being a gelatinous film. Recent studies have confirmed this characteristic, which confers... -
Upper-ocean microstructure data from the tropical Atlantic
SST variability within the Atlantic cold tongue (ACT) region is of climatic relevance for the surrounding continents. A multi cruise data set of microstructure observations is... -
Mixed layer heat and salinity budgets during the onset of the 2011 Atlantic c...
The mixed layer (ML) temperature and salinity changes in the central tropical Atlantic have been studied by a dedicated experiment (Cold Tongue Experiment (CTE)) carried out... -
Biogenic composition of the sea-surface microlayer from a mesocosm study (Ber...
The sea-surface microlayer (SML) is the ocean's uppermost boundary to the atmosphere and in control of climate relevant processes like gas exchange and emission of marine...
