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 |
|
|
304 |
%% CNHbegin |
%% CNHbegin |
305 |
\input{part1/assim_figure} |
\input{part1/assim_figure} |