ic rct stations than at the warm “spring ” ones. This probably results from the enhanced ice permeability as spring arrives, which allows deposition, (2) upwelling and turbulent diffusion, (3) sediment resuspension and lateral advection, and (4) melting sea ice and icebergs (Löscher et al., 1997;...
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| Format: | Text |
| Language: | English |
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| Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.577.830 http://dev.ulb.ac.be/glaciol/articles/Lannuzel_2007_Marine Chemistry_Distribution and biogeochemical behaviour of iron in the East Antarctic sea ice.pdf |
| Summary: | ic rct stations than at the warm “spring ” ones. This probably results from the enhanced ice permeability as spring arrives, which allows deposition, (2) upwelling and turbulent diffusion, (3) sediment resuspension and lateral advection, and (4) melting sea ice and icebergs (Löscher et al., 1997; |
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