Interhemispheric signal transmission in the Atlantic Ocean connects the deep water production regions of both hemispheres. The nature of these interactions and large scale responses to perturbations on time scales of years to millenia have been investigated using a global general circulation model based on the primitive equations coupled to a dynamic-thermodynamic sea ice model with a viscous-plastic rheology. The coupled model reproduces many aspects of today´s oceanic circulation. Testing the model´s sensitivity revealed a strong dependence of the model results from eddy diffusivities, filtering and topographic effects.:p:The internal variability in the ocean-sea ice system has been addressed by analyzing the model results with statistica...
A 1260-year integration generated by the ECHAM1/LSG coupled atmosphere-ocean general circulation mod...
Most CMIP5 (Coupled Model Intercomparison Project Phase 5) models unrealistically form Antarctic Bot...
We investigate the individual and joint decadal variability of Southern Ocean state quantities, such...
Interhemispheric signal transmission in the Atlantic Ocean connects the deep water production region...
Interhemispheric signal transmission in the Atlantic Ocean connects the deep water production region...
Internal multi-centennial variability of open ocean deep convection in the Atlantic sector of the So...
Most of the Southern Ocean (SO) is marginally stably stratified and thus prone to enhanced convectio...
The natural variability of the Weddell Sea variety of Antarctic Bottom Water (AABW) is examined in a...
The response of an ocean general circulation model to the onset of deep-water formation in the North...
The heat and moisture transports by transient eddies in the EMBM are parameterized by diffusion. The...
We investigate the transient response of the global ocean circulation to enhanced freshwater forcing...
A series of experiments with a hybrid model (ocean circulation model with simple atmospheric feedbac...
International audienceRecent studies have proposed the Southern Ocean as the site of large water-mas...
A 250 year simulation of a strongly eddying global version of the Parallel Ocean Program (POP) model...
The response of the upper, warm limb of the thermohaline circulation in the North Atlantic to a rapi...
A 1260-year integration generated by the ECHAM1/LSG coupled atmosphere-ocean general circulation mod...
Most CMIP5 (Coupled Model Intercomparison Project Phase 5) models unrealistically form Antarctic Bot...
We investigate the individual and joint decadal variability of Southern Ocean state quantities, such...
Interhemispheric signal transmission in the Atlantic Ocean connects the deep water production region...
Interhemispheric signal transmission in the Atlantic Ocean connects the deep water production region...
Internal multi-centennial variability of open ocean deep convection in the Atlantic sector of the So...
Most of the Southern Ocean (SO) is marginally stably stratified and thus prone to enhanced convectio...
The natural variability of the Weddell Sea variety of Antarctic Bottom Water (AABW) is examined in a...
The response of an ocean general circulation model to the onset of deep-water formation in the North...
The heat and moisture transports by transient eddies in the EMBM are parameterized by diffusion. The...
We investigate the transient response of the global ocean circulation to enhanced freshwater forcing...
A series of experiments with a hybrid model (ocean circulation model with simple atmospheric feedbac...
International audienceRecent studies have proposed the Southern Ocean as the site of large water-mas...
A 250 year simulation of a strongly eddying global version of the Parallel Ocean Program (POP) model...
The response of the upper, warm limb of the thermohaline circulation in the North Atlantic to a rapi...
A 1260-year integration generated by the ECHAM1/LSG coupled atmosphere-ocean general circulation mod...
Most CMIP5 (Coupled Model Intercomparison Project Phase 5) models unrealistically form Antarctic Bot...
We investigate the individual and joint decadal variability of Southern Ocean state quantities, such...