Abstract: istorical hydrographic data (1940s?2010) show a distinct cross-slope difference of the lower halocline water (LHW) over the Laptev Sea continental margins. Over the slope, the LHW is on average warmer and saltier by 0.2°C ...

Abstract: The diffusive layering (DL) form of double-diffusive convection cools the Atlantic Water (AW) as it circulates around the Arctic Ocean. Large DL steps, with heights of homogeneous layers often greater than 10 m, have been ...

Abstract: yearlong time series from mooring-based high-resolution profiles of water temperature and salinity from the Laptev Sea slope (2003?04; 2686-m depth; 78°26?N, 125°37?E) shows six remarkably persistent staircase layers in ...

Abstract: AbstractThe Eurasian Basin (EB) of the Arctic Ocean is subject to substantial seasonality. We here use data collected between 2013 and 2015 from six moorings across the continental slope in the eastern EB and identify three ...

Abstract: 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 flux from intermediate-depth (~150–900 ...

Abstract: ct available.

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 in recent decades. The AW warming has been uneven ...