We review the geomorphological, sedimentological and chronological evidence for palaeo-
ice streams on the continental shelf of Antarctica and use this information to investigate …

Ice streams influence ice sheet mass balance and stability but key aspects of their behaviour
remain poorly understood. This paper reviews and discusses one very important aspect …

The presence of a complex bedform arrangement on the sea floor of the continental shelf in
the western Amundsen Sea Embayment, West Antarctica, indicates a multi-temporal record …

Ice streams are integral components of an ice sheet's mass balance and directly impact on
sea level. Their flow is governed by processes at the ice‐bed interface which create …

Когда-то, на заре своего зарождения, гляциология рассматривалась как часть
гидрологии, но уже в середине XIX в. выяснилось, что закономерности развития …

Subglacial hydrology in East Antarctica is poorly understood, yet may be critical to the
manner in which ice flows. Data from a new regional airborne geophysical survey (ICECAP) …

Over the past 50 years, the British Antarctic Survey (BAS) has been one of the major
acquirers of aerogeophysical data over Antarctica, providing scientists with gravity, magnetic …

The stability of Antarctic ice sheets and their potential contribution to sea level under
projected future warming remains highly uncertain. The Last Interglacial (135 000–116 000 …

The subglacial environment of the Greenland Ice Sheet (GrIS) is poorly constrained both in
its bulk properties, for example geology, the presence of sediment, and the presence of …

The ice stream geometry and large ice surface velocities at the onset region of the Northeast
Greenland Ice Stream (NEGIS) are not yet well reproduced by ice sheet models. The …