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

Atlantic Water is a major contributor to the largest zonal variability in ocean properties and
air-sea-ice interaction in the Nordic Seas and the European Arctic. Climate change has …

This study investigates the response of four High Arctic catchments with differing proportions
of glacierization to changing climatic conditions. The study area located in SW Spitsbergen …

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 …

The warming of the Arctic climate is well documented, but the mechanisms of Arctic
amplification are still not fully understood. Thus, monitoring of glaciological and …

Dynamic climate changes are particularly apparent in polar regions. Glaciers are retreatng
towards the land at a very fast pace. This study demonstrates the application of the feature …

Monitoring changes in glacial dynamics is essential for understanding the environmental
response to accelerated climate warming in the Arctic. However, geodetic surveys in polar …

In polar regions, glaciers are retreating onto land, gradually widening ice-free coastal
waters, which are known to act as new sinks of atmospheric carbon. However, the …

Frontal ablation is responsible for a large fraction of the mass loss from tidewater glaciers.
The main contributors to frontal ablation are iceberg calving and submarine melting, with …

The areas covered by permafrost in the polar regions are vulnerable to rapid changes in the
current climate. The well-studied near-surface active layer and permafrost zone are in …