OS - Observation-based estimates of volume, heat, and freshwater exchanges between the subpolar North Atlantic interior, its boundary currents, and the atmosphere
Por um escritor misterioso
Last updated 25 março 2025


A shift in the ocean circulation has warmed the subpolar North Atlantic Ocean since 2016

Recent observational advances from the South Atlantic Meridional Overturning Circulation (SAMOC) initiative & GOHSnap: Updates from the field - PhD. Renellys Perez, Prof. Jaime Palter - Universität Hamburg - Lecture2Go

The Arctic Subpolar Gyre sTate Estimate: Description and Assessment of a Data‐Constrained, Dynamically Consistent Ocean‐Sea Ice Estimate for 2002–2017 - Nguyen - 2021 - Journal of Advances in Modeling Earth Systems - Wiley Online Library

Lagrangian Views of the Pathways of the Atlantic Meridional Overturning Circulation - Bower - 2019 - Journal of Geophysical Research: Oceans - Wiley Online Library

Observed mechanisms activating the recent subpolar North Atlantic Warming since 2016 Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences

OS - Observation-based estimates of volume, heat, and freshwater exchanges between the subpolar North Atlantic interior, its boundary currents, and the atmosphere

OS - Observation-based estimates of volume, heat, and freshwater exchanges between the subpolar North Atlantic interior, its boundary currents, and the atmosphere

OS - Observation-based estimates of volume, heat, and freshwater exchanges between the subpolar North Atlantic interior, its boundary currents, and the atmosphere

Interactions between the Arctic Mediterranean and the Atlantic Meridional Overturning Circulation: A Review

Interactions between the Arctic Mediterranean and the Atlantic Meridional Overturning Circulation: A Review

OS - Exceptional freshening and cooling in the eastern subpolar North Atlantic caused by reduced Labrador Sea surface heat loss

Map of the Iceland Basin showing the location of the Overturning in the

Projected Atlantic overturning slow-down is to be compensated by a strengthened South Atlantic subtropical gyre

Bathmetry and circulation near the north Iceland shelf. Schematic

Bathymetric map of subpolar waters between Greenland and Scotland. It
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