Abstract Ice-free areas occupy< 0.5% of Antarctica and are unevenly distributed across the
continent. Terrestrial ecosystem dynamics in ice free areas are strongly influenced by …

Climate change presents challenges for the management of geoheritage at all scales from
individual geosites to whole landscapes, and affecting all areas of the planet. Direct impacts …

Map** accurately vegetation surfaces in space and time in the ice-free areas of Antarctica
can provide important information to quantitatively describe the evolution of their …

Spatio-temporal patterns of glacial retreat determine the intensity of geomorphological,
hydrological, and ecological processes in the ice-free areas of the Antarctic Peninsula …

Uncertainties about landscape evolution under cold, nonglacial conditions raise a question
fundamental to periglacial geomorphology: what and where are periglacial landscapes? To …

The seasonal movement of the zero-degree isotherm across the Southern Ocean and
Antarctic Peninsula drives major changes in the physical and biological processes around …

ABSTRACT This study presents a 1: 25,000 geomorphological map of the northern sector of
Ulu Peninsula, James Ross Island, Antarctic Peninsula. The map covers an area of c. 250 …

The timing and magnitude of Holocene glacial oscillations in most currently ice‐free areas of
Antarctica remain unknown. This work focuses on the recent deglaciation in the northern …

Rock glaciers are periglacial landforms sensitive to climate change, and a harsh
environment for vegetation colonization due to the potential occurrence of surface instability …

Glaciers cover 132 900 km2 around the Antarctic Ice Sheet, but few are subject to annual
mass-balance measurements. Lookalike Glacier and Davies Dome on James Ross Island …