Global warming is not often discussed in the context of light availability within the water
column. However, the light regimes in the Arctic Ocean are controlled by three factors that …

Meltwater streams connect the glacial cryosphere with downstream ecosystems. Dissolved
and particulate matter exported from glacial ecosystems originates from contrasting …

We present a thorough evaluation of the water soluble fraction of the trace element
composition (Ca, Sr, Mg, Na, K, Li, B, Rb, U, Ni, Co, As, Cs, Cd, Mo, Se, Eu, Ba, V, Ge, Ga …

Metals and metalloids in snow on glaciers, depending on the season of deposition, may
come from various sources: local rock dust (erosion of the geological substratum), marine …

Most glaciers worldwide are undergoing climate-forced recession, but the impact of glacier
changes on biogeochemical cycles is unclear. This study examines the influence of …

Glaciers and rock glaciers are key elements of mountain hydrological systems, but their
relative influence on the chemical and isotopic conditions of streams within the river …

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 …

Iron plays a pivotal role in marine primary production and the carbon cycle. Glaciers have
been recognized as a regional iron source to the ocean. Understanding both the …

The shaping of surface water chemistry in the Svalbard Archipelago is strongly dependent
on the geology of the catchment and the process of long-range transport of atmospheric …

Progressive climate change may have unpredictable consequences for the Arctic
environment. Permafrost catchments off the west coast of Svalbard, described as “thin” and …