SOCCO releases its Phase IV Integrated Science and Innovation Strategy: 2022-2027
SOCCO releases its Phase IV Integrated Science and Innovation Strategy: 2022-2027
SOCCO releases its Phase IV Integrated Science and Innovation Strategy: 2022-2027
SOCCO releases its Phase IV Integrated Science and Innovation Strategy: 2022-2027
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The OceanGliders program started in 2016 to support active coordination and enhancement of global glider activity. OceanGliders contributes to the international efforts of the Global Ocean Observation System (GOOS) for Climate, Ocean Health, and Operational Services. It brings together marine scientists and engineers operating gliders around the world: (1) to observe the long-term physical, biogeochemical, and biological ocean processesRead More..

SOCCO releases its Phase IV Integrated Science and Innovation Strategy: 2022-2027
SOCCO releases its Phase IV Integrated Science and Innovation Strategy: 2022-2027
SOCCO releases its Phase IV Integrated Science and Innovation Strategy: 2022-2027
SOCCO releases its Phase IV Integrated Science and Innovation Strategy: 2022-2027
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Active fluorescence measurements can provide rapid, non-intrusive estimates of phytoplankton primary production at high spatial and temporal resolution, but there is uncertainty in converting from electrons to ecologically relevant rates of CO2 assimilation. In this study, we examine the light-dependent rates of photosynthetic electron transport and 13C-uptake in the Atlantic sector of the Southern OceanRead More..

SOCCO releases its Phase IV Integrated Science and Innovation Strategy: 2022-2027
SOCCO releases its Phase IV Integrated Science and Innovation Strategy: 2022-2027
SOCCO releases its Phase IV Integrated Science and Innovation Strategy: 2022-2027
SOCCO releases its Phase IV Integrated Science and Innovation Strategy: 2022-2027
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°The seasonal and sub-seasonal dynamics of iron availability within the sub-Antarctic zone (SAZ; 40–45°S) play an important role in the distribution, biomass and productivity of the phytoplankton community. The variability in iron availability is due to an interplay between winter entrainment, diapycnal diffusion, storm-driven entrainment, atmospheric deposition, iron scavenging and iron recycling processes. Biological observationsRead More..