Ocean tides are the main source of high‐frequency variability in the vertical and horizontal
motion of ice sheets near their marine margins. Floating ice shelves, which occupy about …

ABSTRACT The Arctic Ocean traditionally has been described as an ocean with low
variability and weak turbulence levels. Many years of observations from ice camps and ice …

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 …

A 15-yr duration record of mooring observations from the eastern (> 70° E) Eurasian Basin
(EB) of the Arctic Ocean is used to show and quantify the recently increased oceanic heat …

The loss of Arctic sea ice has emerged as a leading signal of global warming. This, together
with acknowledged impacts on other components of the Earth system, has led to the term …

Abstract Analysis of modern and historical observations demonstrates that the temperature
of the intermediate-depth (150–900 m) Atlantic water (AW) of the Arctic Ocean has increased …

Fine-and microstructure data from a free fall profiler are analysed to test models that relate
the turbulent dissipation rate (ε) to characteristics of the internal wave field. The data were …

We present a comparison of Arctic Ocean hydrographic data sets from the 1990s, with a
focus on changes in the upper few hundred meters of the Eurasian Basin. The most recent …

Turbulence data from three Arctic drift station experiments demonstrate features of turbulent
heat transfer in the oceanic boundary layer. Time series analysis of several w′ T′ records …

Elevated biological concentrations of methylmercury (MeHg), a bioaccumulative neurotoxin,
are observed throughout the Arctic Ocean, but major sources and degradation pathways in …