Will high-resolution global ocean models benefit coupled predictions on short-range to climate timescales?
HT Hewitt, MJ Bell, EP Chassignet, A Czaja, D Ferreira… - Ocean Modelling, 2017 - Elsevier
As the importance of the ocean in the weather and climate system is increasingly
recognised, operational systems are now moving towards coupled prediction not only for …
recognised, operational systems are now moving towards coupled prediction not only for …
The GFDL global ocean and sea ice model OM4. 0: Model description and simulation features
We document the configuration and emergent simulation features from the Geophysical
Fluid Dynamics Laboratory (GFDL) OM4. 0 ocean/sea ice model. OM4 serves as the …
Fluid Dynamics Laboratory (GFDL) OM4. 0 ocean/sea ice model. OM4 serves as the …
Two-timescale response of a large Antarctic ice shelf to climate change
A potentially irreversible threshold in Antarctic ice shelf melting would be crossed if the
ocean cavity beneath the large Filchner–Ronne Ice Shelf were to become flooded with warm …
ocean cavity beneath the large Filchner–Ronne Ice Shelf were to become flooded with warm …
Gateway-driven weakening of ocean gyres leads to Southern Ocean cooling
Declining atmospheric CO2 concentrations are considered the primary driver for the
Cenozoic Greenhouse-Icehouse transition,~ 34 million years ago. A role for tectonically …
Cenozoic Greenhouse-Icehouse transition,~ 34 million years ago. A role for tectonically …
Warm Circumpolar Deep Water transport toward Antarctica driven by local dense water export in canyons
Poleward transport of warm Circumpolar Deep Water (CDW) has been linked to melting of
Antarctic ice shelves. However, even the steady-state spatial distribution and mechanisms of …
Antarctic ice shelves. However, even the steady-state spatial distribution and mechanisms of …
Thermal responses to Antarctic ice shelf melt in an eddy-rich global ocean–sea ice model
The response of near-Antarctic waters to freshening by increased glacial melt is investigated
using a high-resolution (0.1°) global ocean–sea ice model with realistic Antarctic water …
using a high-resolution (0.1°) global ocean–sea ice model with realistic Antarctic water …
Shutdown of Southern Ocean convection controls long-term greenhouse gas-induced warming
A Gjermundsen, A Nummelin, D Olivié, M Bentsen… - Nature …, 2021 - nature.com
The effective climate sensitivity estimates the equilibrium response of near-surface
temperature to doubling atmospheric carbon dioxide concentration and is a widely used …
temperature to doubling atmospheric carbon dioxide concentration and is a widely used …
[HTML][HTML] Transient and equilibrium responses of the Atlantic overturning circulation to warming in coupled climate models: The role of temperature and salinity
The long-term response of the Atlantic meridional overturning circulation (AMOC) to climate
change remains poorly understood, in part due to the computational expense associated …
change remains poorly understood, in part due to the computational expense associated …
Buoyancy forcing dominates the cross-equatorial ocean heat transport response to Northern Hemisphere extratropical cooling
Cross-equatorial ocean heat transport (OHT) changes have been found to damp meridional
shifts of the intertropical convergence zone (ITCZ) induced by hemispheric asymmetries in …
shifts of the intertropical convergence zone (ITCZ) induced by hemispheric asymmetries in …
Wind–and sea‐ice–driven interannual variability of Antarctic Bottom water formation
C Schmidt, AK Morrison… - Journal of Geophysical …, 2023 - Wiley Online Library
Abstract Antarctic Bottom Water (AABW) is a major component of the global overturning
circulation, originating around the Antarctic continental margin. In recent decades AABW has …
circulation, originating around the Antarctic continental margin. In recent decades AABW has …