A nearly continuous survey of the coastline from long. 9–44° W. was carried out during January–February 1977 from the ship of the Norwegian Antarctic Research Expedition, 1976–77. The position of the ice front could be determined within ±200 m by use of an integrated navigation system including a two-channel satellite receiver, in combination with a calibrated radar. Selected points along the coast were determined with a precision of ±10 m, using both the shipborne navigation system and a separate, mobile, two-channel system.
A comparison of the repeated surveys of the position of the ice front reveal a pattern of high-velocity ice streams bounded by slow-moving ice, giving rise to complex strain fields. For example, the Filchner Ice Shelf shows northward movements increasing from nearly zero at long. 44°W. (Gould Bay) to 2 km year−1 at long. 40° W., over a distance of only 90 km. At long. 40° W. the ice front advanced 43 km between 1956 and 1977, and during this period a 20 km ×25 km piece of the ice shelf calved off between long. 42° W. and 43° W. East of 40° W., toward Vahsel Bay, the velocities decrease to around 1 km year−1. Other complicated patterns, with velocities exceeding 1 km year−1 in the fastest sections, are found in several other places along the coast. The larger outflow rates are generally observed west of Kap Norvegia (long. 12° W.) with a major exception at Jutultunga (long. 1° W.), where the velocity exceeds 1 km year−1 over a 60 km wide ice front. The velocity patterns reflect complicated ice dynamics related to the up-stream subglacial topography, and permit identification of zones of varying dynamic activity in the corresponding parts of the inland ice sheet.
Control on the early surveys is provided by those short coastal segments where ice shelf is absent, and generally the positions agree to within 1 km.
The calving is related to the strain patterns, and incipient break-off can be identified 20 years prior to final severing. This final calving is probably a rapid event, triggered by a storm, collision by a large iceberg, or large ocean swells.
The elevation of the ice front was measured at numerous locations by the 1976–77 expedition with a precision better than ±1 m. In general the elevations increase westwards from long. 9° W. to 44° W. Firn density at fixed depth also increases westwards, and consequently the mass of a unit width of the ice front is nearly doubled along this section. The mass outflow across separate coastline segments is calculated and related to the up-stream mass balance.
