Validity of the ice shelf water plume concept beneath Filchner-Ronne Ice Shelf
In winter, brine rejection from sea ice formation and export in the Weddell Sea, offshore of Filchner-Ronne Ice Shelf (FRIS), leads to the formation of High Salinity Shelf Water (HSSW). This dense water mass enters the cavity beneath FRIS by sinking southward down the sloping continental shelf towar...
Main Authors: | , , |
---|---|
Format: | Book Part |
Language: | unknown |
Published: |
FRISP
2006
|
Subjects: | |
Online Access: | https://centaur.reading.ac.uk/35322/ http://folk.uib.no/ngfso/FRISP/frispREP17.html |