Barents Sea Atlantification Driven by a Shift in Atmospheric Synoptic Timescale

dc.contributor.author Robinson Hordoir
dc.contributor.author Heiner Dietze
dc.contributor.author Pål Erik Isachsen
dc.contributor.author Ulrike Loeptien
dc.contributor.author Vahidreza Jahanmard
dc.contributor.author Vidar Lien
dc.contributor.author Anne Britt Sandø
dc.date.accessioned 2025-12-31T13:17:50Z
dc.date.available 2025-12-31T13:17:50Z
dc.date.issued 2025-07-10
dc.description <title>Abstract</title> <p>Climate change impinges on the Arctic Ocean, leading to sea ice loss and poten- tially drastic cascading ecosystem changes. Still, the underlying mechanisms are not yet comprehensively understood. A respective recent process is the Atlantifi- cation, coined to describe the growing influence of warm and salty waters from the Atlantic on the Arctic. A major contributor to this trend is the increasing ocean volume transport from the Nordic Seas to the Barents Sea. Despite its large importance and a multitude of hypotheses that have been put to test, this trend remains mainly unexplained. Here we explore non-linear effects and, for the first time, successfully link the flow trend through the Barents Sea opening to a frequency shift in the atmospheric synoptic.</p>
dc.identifier.doi 10.21203/rs.3.rs-6046335/v1
dc.identifier.uri https://ror.circle-u.eu/handle/123456789/1697247
dc.openaire.affiliation University of Oslo
dc.openaire.collaboration 1
dc.publisher Springer Science and Business Media LLC
dc.rights OPEN
dc.rights.license c_abf2
dc.title Barents Sea Atlantification Driven by a Shift in Atmospheric Synoptic Timescale
dc.type publication

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