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revision 1.14 by cnh, Wed Nov 21 14:13:17 2001 UTC revision 1.15 by cnh, Wed Nov 21 16:33:17 2001 UTC
# Line 295  ocean circulation. An appropriately defi Line 295  ocean circulation. An appropriately defi
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}
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