Biogeochemical modelling of the feedback between ocean biota and climate at polar latitudes

• Other Authors: AADC (owner), AADC, DATA OFFICER (distributor), AADC, DATA OFFICER (custodian), AU/AADC > Australian Antarctic Data Centre, Australia (hasAssociationWith), Australian Antarctic Data Centre (publisher), Australian Antarctic Division (sponsor), CONNELL, DAVE J. (author), GABRIC, ALBERT (collaborator), GABRIC, ALBERT (hasPrincipalInvestigator), Gabric, A. (originator)
• Format: Dataset
• Language: unknown
• Published: Australian Ocean Data Network
• Subjects: oceans; EARTH SCIENCE > OCEANS > OCEAN CHEMISTRY > NUTRIENTS; PIGMENTS > CHLOROPHYLL; dms; sulphur; dimethylsulfide; chlorophyll a; AMD/AU; CEOS; AMD; ARCTIC; OCEAN > ARCTIC OCEAN; SOUTHERN OCEAN; CONTINENT > NORTH AMERICA > GREENLAND; GEOGRAPHIC REGION > POLAR; ARCTIC OCEAN > BARENTS SEA; albedo; Antarc*; Antarctic; Arctic Ocean; Barents Sea; Global warming; Greenland; Sea ice; Southern Ocean
• Online Access: https://researchdata.edu.au/biogeochemical-modelling-feedback-polar-latitudes/2820594

Progress Code: completed Statement: The Dates provided in temporal coverage are approximate only, and represent the beginning and end of the 2004 - 2007 Antarctic seasons. The latitudes and longitudes provided in spatial coverage are approximate only. Metadata record for data from ASAC Project 2584 See the link below for public details on this project. The Southern Ocean plays a significant role in the biogeochemical cycling of sulphur due to high spring-summer fluxes of dimethylsulfide (DMS), particularly south of 60 degrees S. Recent DMS flux perturbation simulations have recently highlighted the key role of the SO between 50-70 degrees S in the DMS-climate feedback hypothesis [Gabric et al., 2003; Gabric et al., 2004]. This project examines the interactions and feedback between marine polar plankton and global climate through the use of biogeochemical and global climate models, and explores the sensitivity of climate to the current and future biogenic production of dimethylsulphide at polar latitudes. This was a modelling project, and as such did not collect any data of its own. Taken from the abstracts of the referenced papers: The global climate is intimately connected to changes in the polar oceans. The variability of sea ice coverage affects deep-water formations and large-scale thermohaline circulation patterns. The polar radiative budget is sensitive to sea-ice loss and consequent surface albedo changes. Aerosols and polar cloud microphysics are crucial players in the radioactive energy balance of the Arctic Ocean. The main biogenic source of sulfate aerosols to the atmosphere above remote seas is dimethylsulfide (DMS). Recent research suggests the flux of DMS to the Arctic atmosphere may change markedly under global warming. This paper describes climate data and DMS production (based on the five years from 1998 to 2002) in the region of the Barents Sea (30-35 degrees E and 70-80 degrees N). A DMS model is introduced together with an updated calibration method. A genetic algorithm is used to ...