Ocean reanalyses combine ocean models, atmospheric forcing fluxes, and observations
using data assimilation to give a four-dimensional description of the ocean. Metrics …

Since 19 October 2016, and in the framework of Copernicus Marine Environment Monitoring
Service (CMEMS), Mercator Ocean has delivered real-time daily services (weekly analyses …

Eastern Fram Strait and the shelf slope region north of Svalbard is dominated by the
advection of warm, salty and nutrient-rich Atlantic Water (AW). This oceanic heat contributes …

Low‐salinity waters in the upper Arctic Ocean, referred to as “freshwaters”, are cold and play
a major role in isolating the sea ice cover from the heat stored in the salty Atlantic Waters …

Arctic sea ice has been in rapid decline the last decade and the Norwegian young sea ICE
(N‐ICE2015) expedition sought to investigate key processes in a thin Arctic sea ice regime …

The global high resolution monitoring and forecasting system PSY4 at Mercator Océan,
initialized in October 2006, has achieved 11 years of global ocean state estimation. Based …

Abstract The northwestern Barents Sea (NW-BS) is a highly productive region within the
transitional zones of an Atlantic to Arctic-dominated marine ecosystem. The steep latitudinal …

Oceanographic observations from the Eurasian Basin north of Svalbard collected between
January and June 2015 from the N‐ICE2015 drifting expedition are presented. The unique …

We investigated wintertime convection evolution in recent years over the Greenland Sea.
This area is a major location regarding dense water production and supply of the lower limb …

Abstract The Atlantic Water (AW) inflow through Fram Strait, largest oceanic heat source to
the Arctic Ocean, undergoes substantial modifications in the Western Nansen Basin (WNB) …