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A geomagnetic observatory is a permanent facility where magnetic declination and inclination are recorded in conjunction with the temporal evolution of the magnetic field components. Polar regions are...
“Deployment of broadband seismic stations on the Antarctica continent” is an ambitious project to improve the spatial resolution of seismic data across the Antarctic Plate and surrounding regions. Sev...
The CASE-IPY project, part of the larger POLENET initiative of geophysical observations for the International Polar Year, was built on our extensive experience of running seismological stations in Ant...
Deception Island is an active volcano located in the south Shetland Islands, Antarctica. It constitutes a natural laboratory to test geophysical instruments in extreme conditions, since they have to e...
We present a detailed analysis of bed roughness beneath Institute and Möller Ice Streams, west Antarctica, using radio-echo sounding data (RES) acquired in the austral summer of 2010/11. We asses...
Th e We st A ntar ct ic ice she et (W AIS) has long bee n con si der ed vulne ra ble to ra pid re trea t and today parts are rapidly losing ice. Projection of future change in WAIS is, however, hampe...
Two ice-dynamic transitions of the Antarctic ice sheet – the boundary of grounded ice features and the freely-floating boundary – are mapped at 15-m resolution by par-ticipants of the International P...
Extension during the middle Cenozoic (43–26 Ma) in the north end of the West Antarctic rift system(WARS) is well constrained by seafloor magnetic anomalies formed at the extinct Adare spreading axis.K...
Meteorological conditions and the statistics for the years 1989-2001 of the Basen nunatak in western Dronning Maud Land are presented. The data are from the Finnish research station Aboa (73°03'S, 1...
Variabilities in the spectral and total (between 300-3000 nm) albedo of snow were studied in the Dronning Maud Land region of Antarctica during the austral summers of 1999/2000 and 2000/2001. The meas...
Subglacial bed conditions exert a signif i cant control on ice stream behavior and evolution, and can be characterized by determining bed roughness from FFT analysis of r adar-imaged basal reflector...

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