The subsidence history of the Greenland-Scotland Ridge (GSR) from subaerial to current ocean depths has been investigated by several studies, and the initial hydrographic opening of the North Polar Seas, “NPS” (Arctic Ocean, Nordic Seas) has been linked to major reorganizations of the global oceans and climate throughout the Neogene (23‒3 Myrs ago). However, the current understanding of the GSR subsidence affecting the hydrographic evolution of the Greenland Scotland Seaway and of the critical GSR depth providing effective water mass exchange between the oceans are largely based on conceptual models. Here, we emulate the GSR subsidence by means of a fully coupled ocean-atmosphere General Circulation Model (GCM) with integrated terrestrial...
On geological time scales, the global ocean circulation is controlled by changes in paleobathymetry,...
[1] A global ice-ocean model shows increasing Atlantic water (AW) inflow at the Iceland-Scotland Rid...
We present a mechanism for self‐sustained ocean circulation changes that cause abrupt temperature ch...
Changes in high latitude ocean gateways and CO2 are thought to be main drivers of Cenozoic climate e...
Changes in high latitude ocean gateways and atmospheric CO2 are thought to be main drivers of Cenozo...
The Greenland-Scotland Ridge (GSR) is a crucial hydrographic barrier for the exchange of water masse...
The Cenozoic history of sea ice in the Northern Hemisphere remains poorly constrained. However, seve...
The Miocene (23.03–5.33 Ma) was a time period with a warmer climate than today. During this period, ...
The Miocene (23.03–5.33 Ma) was a time period with a warmer climate than today. During this period, ...
High latitude ocean gateway changes are thought to play a key role in Cenozoic climate evolution. Ho...
Changes in high latitude ocean gateways are thought to be main drivers of Cenozoic climate evolution...
Changes in the geometry of ocean basins have been influential in driving climate change throughout E...
Changes in the geometry of ocean basins have been influential in driving climate change throughout E...
The modern polar cryosphere reflects an extreme climate state with profound temperature gradients to...
Baroclinic transport and the barotropic effect are two different viewpoints for understanding the me...
On geological time scales, the global ocean circulation is controlled by changes in paleobathymetry,...
[1] A global ice-ocean model shows increasing Atlantic water (AW) inflow at the Iceland-Scotland Rid...
We present a mechanism for self‐sustained ocean circulation changes that cause abrupt temperature ch...
Changes in high latitude ocean gateways and CO2 are thought to be main drivers of Cenozoic climate e...
Changes in high latitude ocean gateways and atmospheric CO2 are thought to be main drivers of Cenozo...
The Greenland-Scotland Ridge (GSR) is a crucial hydrographic barrier for the exchange of water masse...
The Cenozoic history of sea ice in the Northern Hemisphere remains poorly constrained. However, seve...
The Miocene (23.03–5.33 Ma) was a time period with a warmer climate than today. During this period, ...
The Miocene (23.03–5.33 Ma) was a time period with a warmer climate than today. During this period, ...
High latitude ocean gateway changes are thought to play a key role in Cenozoic climate evolution. Ho...
Changes in high latitude ocean gateways are thought to be main drivers of Cenozoic climate evolution...
Changes in the geometry of ocean basins have been influential in driving climate change throughout E...
Changes in the geometry of ocean basins have been influential in driving climate change throughout E...
The modern polar cryosphere reflects an extreme climate state with profound temperature gradients to...
Baroclinic transport and the barotropic effect are two different viewpoints for understanding the me...
On geological time scales, the global ocean circulation is controlled by changes in paleobathymetry,...
[1] A global ice-ocean model shows increasing Atlantic water (AW) inflow at the Iceland-Scotland Rid...
We present a mechanism for self‐sustained ocean circulation changes that cause abrupt temperature ch...