Arctic sea-ice loss is a leading indicator of climate change and can be attributed, in large
part, to atmospheric forcing. Here, we show that recent ice reductions, weakening of the …

Multi-proxy biomarker measurements were applied on two sediment cores (PS51/154,
PS51/159) to reconstruct sea ice cover (IP 25), biological production (brassicasterol …

Continental runoff is a major source of freshwater, nutrients and terrigenous material to the
Arctic Ocean. As such, it influences water column stratification, light attenuation, surface …

Connectivity between the terrestrial and marine environment in the Artic is changing as a
result of climate change, influencing both freshwater budgets, and the supply of carbon to …

Concentrations of dissolved (< 0.2 μm) Fe (DFe) in the Arctic shelf seas and in the surface
waters of the central Arctic Ocean are presented. In the Barents and Kara seas, near‐surface …

A description and assessment of the first release of the Arctic Subpolar gyre sTate Estimate
(ASTE_R1), a data‐constrained ocean‐sea ice model‐data synthesis, is presented …

Recent Sea Ice Decline Did Not Significantly Increase the Total Liquid Freshwater Content of
the Arctic Ocean in: Journal of Climate Volume 32 Issue 1 (2019) Jump to Content Jump to Main …

A summary study on oxygen and carbon stable isotopes in planktonic foraminifera from
Arctic Ocean floor appeared in Marine Geology 20 years ago (Spielhagen and Erlenkeuser …

Absorption coefficients of colored dissolved organic matter (CDOM) were measured together
with salinity, δ18O, and inorganic nutrients across the Fram Strait. A pronounced CDOM …

Extremely low summer sea-ice coverage in the Arctic Ocean in 2007 allowed extensive
sampling and a wide quasi-synoptic hydrographic and δ18O dataset could be collected in …