期刊
JOURNAL OF ADVANCES IN MODELING EARTH SYSTEMS
卷 11, 期 12, 页码 3934-3958出版社
AMER GEOPHYSICAL UNION
DOI: 10.1029/2019MS001805
关键词
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资金
- NASA as part of the SWOT Science Team [NNX16AJ35G]
- NSF [OCE-1553593, OCE-1740648]
- National Science Foundation, Division of Polar Programs [NSF PLR -1425989]
- Foundation BNP Paribas
- Massachusetts Water Resource Authority
- International Argo Program
- NASA [NNX16AJ35G, 902804] Funding Source: Federal RePORTER
Biological productivity in the Southern Ocean is limited by iron availability. Previous studies of iron supply have focused on mixed-layer entrainment and diapycnal fluxes. However, the Southern Ocean is a region highly energetic mesoscale and submesoscale turbulence. Here we investigate the role of eddies in supplying iron to the euphotic zone, using a flat-bottom zonally re-entrant model, configured to represent the Antarctic Circumpolar Current region, that is coupled to a biogeochemical model with a realistic seasonal cycle. Eddies are admitted or suppressed by changing the model's horizontal resolution. We utilize cross spectral analysis and the generalized Omega equation to temporally and spatially decompose the vertical transport attributable to mesoscale and submesoscale motions. Our results suggest that the mesoscale vertical fluxes provide a first-order pathway for transporting iron across the mixing-layer base, where diapycnal mixing is weak, and must be included in modeling the open-Southern Ocean iron budget.
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