Tidal vertical mixing beneath Filchner-Ronne Ice Shelf
High Salinity Shelf Water (HSSW) flowing into the cavity beneath Filchner-Ronne Ice Shelf (FRIS) occupies the lower portion of the water column. Tidal mixing is likely to be a primary mechanism for mixing HSSW up through the water column, where it is transformed through
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| Format: | Text |
| Language: | English |
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| Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.504.8927 http://folk.uib.no/ngfls/frisp/Rep14/makinson_2000.pdf |
| Summary: | High Salinity Shelf Water (HSSW) flowing into the cavity beneath Filchner-Ronne Ice Shelf (FRIS) occupies the lower portion of the water column. Tidal mixing is likely to be a primary mechanism for mixing HSSW up through the water column, where it is transformed through |
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