Evidence for regional climate change in the recent evolution of a high latitude pro-glacial lake

Lake Wilson, a perennially ice-capped, deep (>100 m) lake at 80°S in southern Victoria Land was investigated in January 1993. Water chemistry and physical structure showed three distinct layers; an upper c. 35 m mixed layer of low salinity, moderately turbid water; a less turbid mid layer, 20 m t...

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Veröffentlicht in:Antarctic science 1996-03, Vol.8 (1), p.49-59
Hauptverfasser: Webster, Jenny, Hawes, Ian, Downes, Malcolm, Timperley, Michael, Howard-Williams, Clive
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Sprache:eng
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