The contribution to sea level rise from Patagonian icefields is one of the largest mass losses
outside the large ice sheets of Antarctica and Greenland. However, only a few studies have …

Patagonian icefields are losing volume, and their loss is due partly to rapid changes in their
outlet glaciers that terminate in lakes or the ocean. Despite this key influence from outlet …

For the observation and monitoring of glacier surface velocity (GSV), remote sensing is an
increasingly suitable tool thanks to the high temporal and spatial resolution of the data …

Tidewater calving glaciers can undergo large fluctuations not necessarily in direct response
to climate, but rather owing to complex ice–water interactions at the glacier termini. One …

Fedchenko glacier is by far the largest glacier in the Pamir, Tajikistan. Owing to early
accurate mapping of the glacier it is possible to evaluate glacier changes over eight …

Abstract The Patagonian Ice Fields are known to have undergone rapid retreat of frontal
positions and significant thinning of its glaciers over the past decades. However, surface …

We estimate two-dimensional (2D) glacier surface motion using synthetic aperture radar
(SAR) X-band intensity tracking. It has been observed that the viability of SAR interferometry …

En este estudio se presentan las estimaciones de velocidades superficiales de la cuenca
del glaciar Upsala, Campo de Hielo Patagónico Sur (CHPS) durante la temporada de …

Observations of ice flow velocity with TerraSAR-X were carried out over main outlet glaciers
of the Southern Patagonia Icefield (SPI) since 2008 by means of amplitude correlation …

Glaciers are an important climate indicator due to their sensitive dependence upon local and
regional climate variables, which makes them worthwhile research subjects. A …