Lagrangian views of the pathways of the Atlantic Meridional Overturning Circulation
The Lagrangian method—where current location and intensity are determined by tracking
the movement of flow along its path—is the oldest technique for measuring the ocean …
the movement of flow along its path—is the oldest technique for measuring the ocean …
Mixing and air–sea buoyancy fluxes set the time-mean overturning circulation in the subpolar North Atlantic and Nordic Seas
The overturning streamfunction as measured at the OSNAP (Overturning in the Subpolar
North Atlantic Program) mooring array represents the transformation of warm, salty Atlantic …
North Atlantic Program) mooring array represents the transformation of warm, salty Atlantic …
Formation and pathways of dense water in the Nordic Seas based on a regional inversion
Dense waters formed in the Nordic Seas spill across gaps in the Greenland-Scotland Ridge
into the abyss of the North Atlantic to feed the lower limb of the Atlantic Meridional …
into the abyss of the North Atlantic to feed the lower limb of the Atlantic Meridional …
Sources and upstream pathways of the densest overflow water in the Nordic Seas
Overflow water from the Nordic Seas comprises the deepest limb of the Atlantic Meridional
Overturning Circulation, yet questions remain as to where it is ventilated and how it reaches …
Overturning Circulation, yet questions remain as to where it is ventilated and how it reaches …
The emergence of the North Icelandic Jet and its evolution from northeast Iceland to Denmark Strait
Abstract The North Icelandic Jet (NIJ) is an important source of dense water to the overflow
plume passing through Denmark Strait. The properties, structure, and transport of the NIJ are …
plume passing through Denmark Strait. The properties, structure, and transport of the NIJ are …
Along‐stream, seasonal, and interannual variability of the North Icelandic Irminger Current and East Icelandic Current around Iceland
M Casanova‐Masjoan… - Journal of …, 2020 - Wiley Online Library
Data from repeat hydrographic surveys over the 25‐year period 1993 to 2017, together with
satellite altimetry data, are used to quantify the temporal and spatial variability of the North …
satellite altimetry data, are used to quantify the temporal and spatial variability of the North …
The Iceland-Faroe Slope Jet: a conduit for dense water toward the Faroe Bank Channel overflow
Dense water from the Nordic Seas passes through the Faroe Bank Channel and supplies
the lower limb of the Atlantic Meridional Overturning Circulation, a critical component of the …
the lower limb of the Atlantic Meridional Overturning Circulation, a critical component of the …
Water mass transformation in the Iceland Sea: Contrasting two winters separated by four decades
Dense water masses formed in the Nordic Seas flow across the Greenland–Scotland Ridge
and contribute substantially to the lower limb of the Atlantic Meridional Overturning …
and contribute substantially to the lower limb of the Atlantic Meridional Overturning …
Evolution and transformation of the North Icelandic Irminger Current along the North Iceland shelf
Abstract The North Icelandic Irminger Current (NIIC) flowing northward through Denmark
Strait is the main source of salt and heat to the north Iceland shelf. We quantify its along …
Strait is the main source of salt and heat to the north Iceland shelf. We quantify its along …
Lagrangian perspective on the origins of Denmark Strait Overflow
Abstract The Denmark Strait Overflow (DSO) is an important contributor to the lower limb of
the Atlantic meridional overturning circulation (AMOC). Determining DSO formation and its …
the Atlantic meridional overturning circulation (AMOC). Determining DSO formation and its …