66-year run of the channel-ocean version of the MAOOAM model with 40 variables, and parameters h = 1000 m, n= 1.5, and C = 0.01 kg / m^2 /s. Shown are the geopotential height difference between two locations in the spatial domain, a three-dimensional projection of the attractor of the system for the variables (ψa,1, ψo,1 To,1), and four panels representing the solution in the spatial domain. The spatial view is centered at the South pole.

2019

Royal Meteorological Institute of Belgium

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66-year run of the channel-ocean version of the MAOOAM model with 40 variables, and parameters h = 1000 m, n= 1.7, and C = 0.02 kg / m^2 /s. Shown are the geopotential height difference between two locations in the spatial domain, a three-dimensional projection of the attractor of the system for the variables (ψa,1, ψo,1 To,1), and four panels representing the solution in the spatial domain. The spatial view is centered at the South pole.

2019

Royal Meteorological Institute of Belgium

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66-year run of the channel-ocean version of the MAOOAM model with 40 variables, and parameters h = 1000 m, n= 1.7, and C = 0.027 kg / m^2 /s. Shown are the geopotential height difference between two locations in the spatial domain, a three-dimensional projection of the attractor of the system for the variables (ψa,1, ψo,1 To,1), and four panels representing the solution in the spatial domain. The spatial view is centered at the South pole.

2019

Royal Meteorological Institute of Belgium

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66-year run of the channel-ocean version of the MAOOAM model with 40 variables, and parameters h = 1000 m, n= 1.7, and C = 0.01 kg / m^2 /s. Shown are the geopotential height difference between two locations in the spatial domain, a three-dimensional projection of the attractor of the system for the variables (ψa,1, ψo,1 To,1), and four panels representing the solution in the spatial domain. The spatial view is centered at the South pole.

2019

Royal Meteorological Institute of Belgium

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66-year run of the channel-ocean version of the MAOOAM model with 40 variables, and parameters h = 1000 m, n= 1.5, and C = 0.012 kg / m^2 /s. Shown are the geopotential height difference between two locations in the spatial domain, a three-dimensional projection of the attractor of the system for the variables (ψa,1, ψo,1 To,1), and four panels representing the solution in the spatial domain. The spatial view is centered at the South pole.

2019

Royal Meteorological Institute of Belgium

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132-year run of the channel-ocean version of the MAOOAM model with 40 variables, and parameters h = 1000 m, n= 1.7, and C = 0.016 kg / m^2 /s. Shown are the geopotential height difference between two locations in the spatial domain, a three-dimensional projection of the attractor of the system for the variables (ψa,1, ψo,1 To,1), and four panels representing the solution in the spatial domain. The spatial view is centered at the South pole.

2019

Royal Meteorological Institute of Belgium

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66-year run of the channel-ocean version of the MAOOAM model with 40 variables, and parameters h = 1000 m, n= 1.5, and C = 0.016 kg / m^2 /s. Shown are the geopotential height difference between two locations in the spatial domain, a three-dimensional projection of the attractor of the system for the variables (ψa,1, ψo,1 To,1), and four panels representing the solution in the spatial domain. The spatial view is centered at the South pole.

2019

Royal Meteorological Institute of Belgium

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