Glaciers draining to the Hornsund basin (southern Spitsbergen, Svalbard) have experienced
a significant retreat and mass volume loss over the last decades, increasing the input of …

Abstract Changes in the properties and dynamics of tidewater glacier systems are key
indicators of the state of Arctic climate and environment. Calving of tidewater glacier fronts is …

OWCZAREK Z., STACHOWSKA-KAMIŃSKA Z., KOSTRZEWA O., SZCZYPIŃSKA M., 2024.
Progress in Arctic coastal geomorphological research in times of rapid climate warming …

In Svalbard, the rapid glacier retreat observed since the end of the Little Ice Age (LIA) has
transformed the geomorphology and sediment budgets of glacial forelands, river valleys …

The Arctic is a region undergoing continuous and significant changes in land relief due to
different glaciological, geomorphological and hydrogeological processes. To study those …

Glacierised coasts undergo faster geomorphic processes than unglaciated ones. We have
studied changes of the coastal area in southern Svalbard with the glacier bridge between …

The mechanism of glacier recession and its climatic controls are complex processes that
differ across the Arctic region. Here, we investigate factors influencing front variations of …

In this study, we assess the accuracy and precision of digital elevation models (DEM)
retrieved from aerial photographs taken in 2011 and from Very High Resolution satellite …

Many Arctic marine‐terminating glaciers have undergone rapid retreats in recent decades.
Seasonal and year‐to‐year variations in terminus position act on all tidewater glaciers, but …

Tidewater glaciers on the east coast of Svalbard were examined for surface elevation
changes and retreat rate. An archival digital elevation model (DEM) from 1970 (generated …