The importance of the Weddell Gyre has long been recognized, but observation has been hindered by its sea ice cover. The Weddell Gyre is nearly completely covered by sea ice in the winter, marking the greatest latitudinal range of the seasonal sea ice around Antarctica. During the 1980's a series of winter and spring expeditions (Somov-81; Polarstern-86, 89; Fedorov-89) provided a more precise view of the coupling of the deep water with the winter mixed layer and its significant impact on seasonal sea ice thickness. Along the western rim of the Weddell Gyre the high concentration of perennial sea ice has hindered even basic exploration of this important region.
Observations from ships are essentially non-existent in the western Weddell (west of 48°W; south of 65°S). A vast region stretching westward to Antarctic Peninsula is largely unexplored, except by satellite borne sensors, recent aircraft based geophysical observations and instrumented drifters placed on the ice. A range of very basic questions exist that can only be addressed with detailed in situ observations of the environmental conditions. Fundamental questions include: why is there an extensive all year ice cover in the western Weddell? how climatically stable is it? how do the ocean processes along the western rim of the Weddell Gyre contribute to the formation or further modification of antarctic bottom water? Even such a basic issue as the location of the continental slope was not resolved: LaBrecque and Ghidella, this issue, using satellite and aircraft data place the eastern continental margin of Antarctic Peninsula about 100 kilometers to the west of position shown on the GEBCO map.
An effective way to gather extensive observations in the ice cluttered western Weddell is to borrow a successful method from the Arctic: deployment of a scientific station on a drifting ice floe. In 1988 the concept for the US/USSR Ice Station Weddell (ISW), the first ice station of the Southern Ocean was initiated, with detailed planning in 1989-1991 and field deployment in 1992. The extensive experience of Russia and the United States in ice station operation formed a natural basis for a collaborative effort to meet the many challenges of establishing a scientific ice station in an unexplored part of the southern ocean.
In the spirit of basic exploration of an unknown region the science program spanned many disciplines. Included were measurements of full water column thermohaline and tracer fields; current measurements; estimations of turbulent fluxes within the oceanic and atmospheric planetary boundary layers; sea ice physical, chemical and biological characteristics; sea ice dynamics; and water column biology. US and Russian science programs complimented each other to yield a more complete picture of the environment. Observations were made at the ISW site, from remote instrumented drifters, from helicopters and from the ships associated with the various phases of the work (Fig. 1). The ISW drifted roughly along 53°W at a northward drift rate of 6.2 km/day between 71.4°S and 65.8°S, experiencing temperatures mostly about -25°C, but getting as low as -36°C.
The US-USSR Ice Station Weddell (ISW) may best be summarized by quoting
the closing statement:
"Tuesday 9 June 1992 at 65.63 deg S and 52.41 deg W
Aboard R/V Akademik Fedorov and R/V Nathaniel B. Palmer.
Chairman of the
Soviet Antarctic Expedition
Chief Scientist for
Ice Station Weddell
V. V. Lukin Arnold L. Gordon
Designed by: Bruce Huber bhuber@ldeo.colubmia.edu
Lamont-Doherty Earth Observatory of Columbia University