This paper summarizes the most significant snow-related research that has been conducted
in Svalbard. Most of the research has been performed during the 1990s and includes …

The spatial distribution of snow thickness on glaciers is driven by a set of clima− tological,
meteorological, topographical and orographic conditions. This work presents re− sults of …

Understanding glacier drainage system behaviour and its response to increased meltwater
production faces several challenges in the High Arctic because many glaciers are …

This paper presents a detailed study of melting processes conducted on Hansbreen-a
tidewater glacier terminating in the Hornsund fjord, Spitsbergen. The fieldwork was carried …

Glacier naledi are extrusive ice masses that appear in front of glaciers as a consequence of
refreezing of meltwater seepage during the accumulation season. These structures provide …

We present a detailed study on snow cover on six different glaciers in southern Spitsbergen,
Svalbard: Amundsenisen, Flatbreen, Hansbreen, Nannbreen, Storbreen and …

River runoff variability in the Scott River catchment in the summer seasons 2012 and 2013
has been presented in comparison to the multiannual river runoff in 1986–2009. Both in …

One of the main controls on the net mass change of land‐terminating Arctic glaciers is the
magnitude and distribution of snow accumulation. In Dickson Land, region of Svalbard with …

Icing fields are common in Svalbard and very diverse with respect to shape. The occurrence
and spatial structure of icing fields in front of glaciers were analysed using aerial …

The general objective of this research has been to identify the factors and condi− tions of
migration of CaCO3 within glaciers and their marginal zones in Svalbard. Special attention …