Swida-RINGS

An airborne campaign to map and investigate most of the major outlet glaciers of Antarctica.

Swida-RINGS

Circumnavigation Science Swida-RINGS


RINGS is a recently approved SCAR project activity, aimed primarily at understanding the mass balance of Antarctica, and provide independent data to rectify long-standing discrepancies between two space-based methods (gravity changes vs elevation changes). This is done by providing key data along the grounding line of Antarctica for the 3rd “input-output method”, where the volume of ice lost through “gates” along the grounding line zone can be determined once the ice thicknesses are known; many areas, especially in East Antarctica, lack such data.

Quick look of a Radar Example from Enderby Land

The instrument Twin-Otter of the circumnavigation (“SWIDA-RINGS”) carries a broad suite of instruments from University of Kansas, Danish DTU-Space and Swiss EPFL instruments: deep radar sounding for measuring the ice of the ice (up to 4 km), a snow radar for mapping the upper yearly snow layers (down to 30-40 m), gravity sensors to supplement the deep radar and giving information on sub-ice geology, laser scanning for measuring the ice surface (at cm-level accuracy), and atmospheric sensors for aerosol and chemical tracers in the pristine Antarctic atmosphere. The Twin-Otter setup is compact and efficient (two racks only), and will produce unique data, serving as a backbone for other RINGS efforts in the coming years.

The black line delineates completed radar survey transects, representing successfully acquired glaciological data, while the yellow line indicates planned survey segments yet to be executed.
Front Geodetic and Atmosphere Rack setup inside the Survey Aircraft, C-FDHB
Professor Carl Leuschen operating RDS electronics, middle Snow Radar, and top monitor/laptop.
Linking Airborne Gravity to Ground References