TY - JOUR
T1 - Algae River
T2 - An extensive drainage system in the Bunger Hills, East Antarctica
AU - Gibson, John A.E.
AU - Gore, Damian B.
AU - Kaup, Enn
N1 - Copyright 2002 Cambridge University Press. Reprinted from Polar record.
PY - 2002
Y1 - 2002
N2 - An extensive terrestrial drainage system, centred on Algae Lake in southern Bunger Hills, is described. The 25-km-long Algae River is the third longest known in Antarctica after Onyx River (Wright Valley, Victoria Land) and Druzhby River (Vestfold Hills, Queen Elizabeth Land). Algae River receives meltwater from the Antarctic ice sheet, Apfel Glacier, and ephemeral and permanent snow banks in the ice-free area of the Bunger Hills. Water flows through a series of epiglacial lakes before reaching the extensive Algae Lake, which in turn has an outlet to Transkriptsii Gulf, a largely fresh-water, tidal epishelf lake connected to the ocean under the Edisto Ice Tongue and Shackleton Ice Shelf. Total flow from Algae Lake was estimated to be greater than 1 x 107 m3 a-1 from data collected in the 1986/87 summer. Some portions of the drainage system that were flowing during the 1946/47, 1985/86, 1986/87, 1994/95, 1995/96, and 1998/99 summers were not flowing during the 1999/2000 summer, indicating the variable nature of discharge in the river and emphasising that parts of the drainage network may become disconnected readily.
AB - An extensive terrestrial drainage system, centred on Algae Lake in southern Bunger Hills, is described. The 25-km-long Algae River is the third longest known in Antarctica after Onyx River (Wright Valley, Victoria Land) and Druzhby River (Vestfold Hills, Queen Elizabeth Land). Algae River receives meltwater from the Antarctic ice sheet, Apfel Glacier, and ephemeral and permanent snow banks in the ice-free area of the Bunger Hills. Water flows through a series of epiglacial lakes before reaching the extensive Algae Lake, which in turn has an outlet to Transkriptsii Gulf, a largely fresh-water, tidal epishelf lake connected to the ocean under the Edisto Ice Tongue and Shackleton Ice Shelf. Total flow from Algae Lake was estimated to be greater than 1 x 107 m3 a-1 from data collected in the 1986/87 summer. Some portions of the drainage system that were flowing during the 1946/47, 1985/86, 1986/87, 1994/95, 1995/96, and 1998/99 summers were not flowing during the 1999/2000 summer, indicating the variable nature of discharge in the river and emphasising that parts of the drainage network may become disconnected readily.
UR - http://www.scopus.com/inward/record.url?scp=0036228351&partnerID=8YFLogxK
U2 - 10.1017/S0032247400017526
DO - 10.1017/S0032247400017526
M3 - Article
AN - SCOPUS:0036228351
SN - 0032-2474
VL - 38
SP - 141
EP - 152
JO - Polar Record
JF - Polar Record
IS - 205
ER -