Vertical mixing in the Atlantic Ocean during the Last Glacial Maximum may have been enhanced, not reduced, due to more vigorous tidal dissipation, suggest an ensemble of ocean simulations and glacial sediment carbon isotope records
A common conception of the deep ocean during ice age episodes is that the upper circulation cell in ...
The structure of the glacial ocean was significantly different to that of the present day with inter...
Changes in deep ocean ventilation are commonly invoked as the primary cause of lower glacial atmosph...
UVic model simulations to Wilmes et al. (2021), Enhanced vertical mixing in the glacial ocean infer...
affected by both local/regional circulation and by global shifts in the mean isotopic value of the o...
In this study we assimilate measurements of stable carbon isotope compositions #delta#"1"3...
Increased carbon sequestration in the ocean subsurface is commonly assumed to have been one of the m...
A series of Last Glacial Maximum (LGM) marine carbon cycle sensitivity experiments is conducted to ...
Atmospheric CO₂ was ~90 ppmv lower at the Last Glacial Maximum (LGM) compared to the late Holocene, ...
Due to lower sea levels during the Last Glacial Maximum (LGM), tidal energy dissipation was shifted ...
A series of simulations are conducted with a global climate model of intermediate complexity (MoBidi...
Graduation date: June 12, 2017During the Last Glacial Maximum (LGM, ∼ 21 ky before present) the atmo...
Despite its importance for climate and the carbon cycle, the deep ocean circulation during the Last ...
International audienceDespite its role in heat, salt, and nutrient transport, the state of the Atlan...
<p>While paleoproxy records and modelling studies consistently suggest that North Atlantic&...
A common conception of the deep ocean during ice age episodes is that the upper circulation cell in ...
The structure of the glacial ocean was significantly different to that of the present day with inter...
Changes in deep ocean ventilation are commonly invoked as the primary cause of lower glacial atmosph...
UVic model simulations to Wilmes et al. (2021), Enhanced vertical mixing in the glacial ocean infer...
affected by both local/regional circulation and by global shifts in the mean isotopic value of the o...
In this study we assimilate measurements of stable carbon isotope compositions #delta#"1"3...
Increased carbon sequestration in the ocean subsurface is commonly assumed to have been one of the m...
A series of Last Glacial Maximum (LGM) marine carbon cycle sensitivity experiments is conducted to ...
Atmospheric CO₂ was ~90 ppmv lower at the Last Glacial Maximum (LGM) compared to the late Holocene, ...
Due to lower sea levels during the Last Glacial Maximum (LGM), tidal energy dissipation was shifted ...
A series of simulations are conducted with a global climate model of intermediate complexity (MoBidi...
Graduation date: June 12, 2017During the Last Glacial Maximum (LGM, ∼ 21 ky before present) the atmo...
Despite its importance for climate and the carbon cycle, the deep ocean circulation during the Last ...
International audienceDespite its role in heat, salt, and nutrient transport, the state of the Atlan...
<p>While paleoproxy records and modelling studies consistently suggest that North Atlantic&...
A common conception of the deep ocean during ice age episodes is that the upper circulation cell in ...
The structure of the glacial ocean was significantly different to that of the present day with inter...
Changes in deep ocean ventilation are commonly invoked as the primary cause of lower glacial atmosph...
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