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We illustrate systematic oscillations of the global average temperature in forecasts produced by the NCAR Community Climate Model (CCM). These oscillations are not simple linear oscillations associated with normal modes calculated about a state of rest Rather they result from an interaction between zonal-average gravity modes and zonal-average Rossby modes. Their amplitudes are related to the difference between the initial conditions and the model's average climate.
We illustrate systematic oscillations of the global average temperature in forecasts produced by the NCAR Community Climate Model (CCM). These oscillations are not simple linear oscillations associated with normal modes calculated about a state of rest Rather they result from an interaction between zonal-average gravity modes and zonal-average Rossby modes. Their amplitudes are related to the difference between the initial conditions and the model's average climate.
| All Time | Past Year | Past 30 Days | |
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| Abstract Views | 0 | 0 | 0 |
| Full Text Views | 52 | 12 | 0 |
| PDF Downloads | 22 | 5 | 0 |
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