put into the development of new models approaches for phytoplankton physiology, iron chemistry and phytoplankton community composition (phytoplankton functional types). The models have been validated with [...] the export of biogenic carbon with the sinking phytoplankton from the sea surface to the ocean floor at about 4000 m depth (EIFEX). We determined phytoplankton species succession, decline of the fertilised [...] masses were quantified as were the carbon budgets of the developing plankton blooms. Further phytoplankton species succession, decline of the fertilised bloom, its sinking through the water column to the

Peter Henry Burkill Director, Sir Alister Hardy Foundation for Ocean Science marine biology, phytoplankton Prof. Dr. Karen J. Heywood University of East Anglia, School of Environmental Sciences physical [...] exchange at a Siberian permafrost landscape 16:40 - 17:00 Effects of CO2 and iron on Antarctic phytoplankton S. Trimborn 17:00 - 17:20 Ocean-atmosphere-ice sheet interactions in the North Atlantic region

Peter Henry Burkill Director, Sir Alister Hardy Foundation for Ocean Science marine biology, phytoplankton 9 Dr. John Campbell 2 Technical Director, Oil and Gas Producers geochemistry, environmental advocacy

ivity and finally atmospheric signal may be expected, reflecting the impact of winter SIE on phytoplankton bloom after retreat of the sea ice in spring (Curran et al., 2003; Abram et al., 2007). Nevertheless

ivity and finally atmospheric signal may be expected, reflecting the impact of winter SIE on phytoplankton bloom after retreat of the sea ice in spring (Curran et al., 2003; Abram et al., 2007). Nevertheless

ivity and finally atmospheric signal may be expected, reflecting the impact of winter SIE on phytoplankton bloom after retreat of the sea ice in spring (Curran et al., 2003; Abram et al., 2007). Nevertheless

Jones, G., and Trevena, A. J.: Correlations between the satellite-derived seasonal cycles of phytoplankton biomass and aerosol opti- cal depth in the Southern Ocean: Evidence for the influ- ence of sea

methane and phytoplankton: interactions along a north-south transit in the western Pacific Ocean. Biogeosciences, 10, 3297-3311. 2 Phytoplankton functional types from space (S4-SR-6) Phytoplankton contributes [...] Synergy R & D Study 4: Phytoplankton Functional Types Requirements Baseline Document Version: 2 Doc: SEOM-SynSenPFT-RB-D1.1 Date: 10 Mar 2015 1 SY-4Sci Synergy R & D Study 4: Phytoplankton Functional Types [...] 19 Figure 5. Monthly Chla for specific phytoplankton groups – March 2007. ............................. 22 Figure 6. Seasonal amplitude of the large phytoplankton diatoms (PhytoDOAS, PHYSAT) / (all others)

Multispectral Sentinel-Measurements to Determine Phytoplankton Functional Types at Best Spatial and Temporal Resolution (SynSenPFT) Motivation: Different phytoplankton groups have different roles in the biogeochemical [...] situ data of phytoplankton pigments Diagnostic Pigment Analysis10 f-PFTs Fit function applied to satellite Chla data Chla conc. of PFTs 3 Validation and intercomparison with phytoplankton size classes [...] pigments specific to phytoplankton functional types. Biogeosciences 8, 311–327. Soppa, M. A., Hirata, T., et al. 2014. Global retrieval of diatoms abundance based on phytoplankton pigments and satellite

to PhytoDOAS method for identication of major phytoplankton groups using hyper-spectral data. Ocean Sciences 8:1055-1070 Sadeghi A (2012) Phytoplankton Functional Groups from Hyperspectral Satellite Data [...] various parameters characterizing phytoplankton and the underwater light field from SCIAMACHY hyperspectral Data Specific (upper) and differential absorption of phytoplankton groups (lower), fitted with PhytoDOAS [...] Availability (E0) DOAS applied to Phytoplankton and to oceanic inelastic processes: based on Beer-Lambert-Law & aims to fulfill the minimization Atmosphere Polynom Phytoplankton Inelastic scattering, water Satellite