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The size-frequency distribution of CSP(2-16µm) in Aelotron experiment 2014
This dataset has no description
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The size-frequency distribution of TEP(2-16µm) in Aelotron experiment 2014
This dataset has no description
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Surface microlayer data during KOSMOS 2011 mesocosm experiment in the Raunefjord
This dataset has no description
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Noble gases measured on water bottle samples during METEOR cruise M68/3
This dataset has no description
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Noble gases measured on water bottle samples during L'Atalante cruise ATA3
This dataset has no description
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Noble gases measured on water bottle samples during Maria S. Merian cruise MS...
The eastern equatorial Atlantic is on of the world's most important upwelling regions. As vertical velocities are too small to be measured directly, they have to be inferred by... -
Noble gases measured on water bottle samples during Maria S. Merian cruise MS...
During the cruise MSM18/2, 307 helium samples in copper tubes were taken, mainly from the mixed layer and the upper thermocline. These samples will be analysed with respect to... -
Noble gas measured on water bottle samples during L'Atalante cruise ATA4
See "Further details:" for information on measurement technique. -
Hydrochemistry measured on water bottle samples during L'Atalante cruise ATA03
This dataset has no description
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Physical oceanography during L'Atalante cruise ATA03
Cruise = Atalante IFM-GEOMAR 3 2008,Ship = NO Atalante,Expocode = 35A320080204,Version = 0.22 used on 2012/03/19 11:26:34,Release = 4,Castpart = down,nc_data_set_type =... -
Effect of wind speed on the size distribution of gel particles in the sea sur...
Gel particles, such as transparent exopolymer particles (TEP) and Coomassie stainable particles (CSP), are important organic components in the sea surface microlayer (SML).... -
Time series of ice nuclei concentration at Cape Verde
Cumulative ice nuclei concentration as function of temperature determined using filter samples collected at the Cape Verde Atmospheric Observatory. Samples cover the year... -
Negligible effects of ocean acidification on Eurytemora affinis
Ocean acidification is caused by increasing amounts of carbon dioxide dissolving in the oceans leading to lower seawater pH. We studied the effects of lowered pH on the calanoid... -
KOSMOS Finland 2012 mesocosm study: ciliate and mesozooplankton community, pr...
Community approaches investigating ocean acidification (OA) effects suggest a high tolerance of micro- and mesozooplankton to carbonate chemistry changes expected to occur... -
Impact of CO2 enrichment on organic matter dynamics during nutrient induced c...
A mesocosm experiment was conducted to investigate the impact of rising fCO2 on the build-up and decline of organic matter during coastal phytoplankton blooms. Five mesocosms... -
The organic sea-surface microlayer in the upwelling region off the coast of P...
The sea-surface microlayer (SML) is at the upper- most surface of the ocean, linking the hydrosphere with the atmosphere. The presence and enrichment of organic compounds in the... -
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... -
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... -
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... -
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...
