Microwave observation of the Weddell polynya

Satellite microwave image data from Nimbus 5 of the Weddell Sea are examined for the years 1973-77. During the winters of 1974, 1975 and 1976 a polynya or ice-enclosed open water area is observed. It has an area 200,000-300,000 sq km and is observed drifting west at about 1 cm/s in the Weddell Sea ice pack. The long-term and short-term behavior of the polynya margin and the regional ice concentration are interpreted in light of several oceanographic and meteorological theories explaining the circulation relevant to its origin, stability and role. It is concluded that water column stability preconditioning alone is a necessary but not sufficient condition for the existence of the polynya.