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...

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Bibliographic Details
Main Authors: Holland, P.R, Feltham, D.L, Jenkins, A
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