119 |
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120 |
Hill, C, Adcroft,A., Jamous,D., and J. Marshall, (1999) |
Hill, C, Adcroft,A., Jamous,D., and J. Marshall, (1999) |
121 |
A Strategy for Terascale Climate Modeling. |
A Strategy for Terascale Climate Modeling. |
122 |
In Proceedings of the Eight ECMWF Workshop on the Use of Parallel Processors |
In Proceedings of the Eighth ECMWF Workshop on the Use of Parallel Processors |
123 |
in Meteorology |
in Meteorology, pages 406-425 |
124 |
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World Scientific Publishing Co: UK |
125 |
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126 |
Marotzke, J, Giering,R., Zhang, K.Q., Stammer,D., Hill,C., and T.Lee, (1999) |
Marotzke, J, Giering,R., Zhang, K.Q., Stammer,D., Hill,C., and T.Lee, (1999) |
127 |
Construction of the adjoint MIT ocean general circulation model and |
Construction of the adjoint MIT ocean general circulation model and |
295 |
the departure of the model from observations (both remotely sensed and |
the departure of the model from observations (both remotely sensed and |
296 |
in-situ) over an interval of time, is minimized by adjusting `control |
in-situ) over an interval of time, is minimized by adjusting `control |
297 |
parameters' such as air-sea fluxes, the wind field, the initial conditions |
parameters' such as air-sea fluxes, the wind field, the initial conditions |
298 |
etc. Figure \ref{fig:assimilated-globes} shows an estimate of the time-mean |
etc. Figure \ref{fig:assimilated-globes} shows the large scale planetary |
299 |
surface elevation of the ocean obtained by bringing the model in to |
circulation and a Hopf-Muller plot of Equatorial sea-surface height. |
300 |
|
Both are obtained from assimilation bringing the model in to |
301 |
consistency with altimetric and in-situ observations over the period |
consistency with altimetric and in-situ observations over the period |
302 |
1992-1997. {\bf CHANGE THIS TEXT - FIG FROM PATRICK/CARL/DETLEF} |
1992-1997. |
303 |
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304 |
%% CNHbegin |
%% CNHbegin |
305 |
\input{part1/assim_figure} |
\input{part1/assim_figure} |