Modeling ocean processes below Fimbulisen, Antarctica

Lars H. Smedsrud*, Adrian Jenkins, David M. Holland, Ole A. Nøst

*Corresponding author for this work

Research output: Contribution to journalArticlepeer-review

39 Citations (Scopus)


[1] Model simulations of circulation and melting beneath Fimbulisen, Antarctica, obtained using an isopycnic coordinate ocean model, are presented. Model results compare well with available observations of currents and hydrography in the open ocean to the north of Fimbulisen and suggest that Warm Deep Water exists above the level of a sub‐ice‐shelf bedrock sill, the principal pathway for warm waters to enter the sub‐ice‐shelf cavity. The model shows a southward inflow of Warm Deep Water over this sill and into the cavity, producing a mean cavity temperature close to −1.0°C. This leads to high levels of basal melting (>10 m/a) at the grounding line of Jutulstraumen and an average melting over the ice shelf base close to 1.9 m/a. The southward inflow is a compensating flow caused by the northward outflow of fresh, cold water produced by the basal melting. Results on inflow and melting are difficult to validate since no in situ measurements yet exist in the cavity. If such high melt rates are realistic, the mass balance of Fimbulisen must be significantly negative, and the ice shelves along Dronning Maud Land must contribute about 4.4 mSv of melt water to the Weddell Sea, about 15% of the total Antarctic meltwater input to the Southern Ocean.
Original languageEnglish
Article numberC01007
Number of pages13
JournalJournal of Geophysical Research
Issue numberC1
Early online date18 Jan 2006
Publication statusPublished - Jan 2006
Externally publishedYes


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