Premium
A late spring surge in the open water of the Antarctic sea ice pack
Author(s) -
Watkins Andrew B.,
Simmonds Ian
Publication year - 1999
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/1999gl900292
Subject(s) - sea ice , geology , spring (device) , oceanography , climatology , fast ice , antarctic sea ice , arctic ice pack , open water , trough (economics) , surge , plateau (mathematics) , ice shelf , drift ice , cryosphere , environmental science , geomorphology , mechanical engineering , mathematical analysis , mathematics , engineering , economics , macroeconomics
Mean annual cycles of open water area within the Antarctic sea ice pack are presented for 1978–87 and 1987–97, compiled using mean daily data. A minimum of the open water area occurs in mid February, followed by a steady increase until a plateau is established in October, before a sudden surge in early November to a peak of 4.5 × 10 6 km². As this Antarctic Open water Surge (AOS) occurs on timescales of around one month, its temporal structure only becomes truly clear when using daily means. The AOS is shown to be the result of the relative timings of the sea ice area and extent annual cycles. It is suggested these reflect the late spring crossing of the Antarctic circumpolar trough over the sea ice edge, thus shifting the dominant winds (Ekman forcing) from westerly (northerly) to easterly (southerly).