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Home > Newsevents > Training > Rcourse_notes > DATA_ASSIMILATION > ASSIM_CONCEPTS >  
   

Data assimilation concepts and methods
March 1999

By F. Bouttier and P. Courtier


1. Basic concepts in data assimilation
2. The state vector, control space and observations
3. The modelling of errors
4. Statistical interpolation with least-squares estimation
5. A simple scalar illustration of least-squares estimation
6. Models of error covariance
7. Optimal interpolation (OI) analysis
8. Three-dimensional variational analysis (3D-Var)
9. 1D-Var and other variational analysis systems
10. Four-dimensional variational assimilation (4D-Var)
11. Estimating the quality of the analysis
12. Implementation techniques
13. Dual formulation of 3D/4D-Var (PSAS)
14. The extended Kalman filter (EKF)
15. Conclusion
Appendix A. A primer on linear matrix algebra
Appendix B. Practical adjoint coding
Appendix C. Exercises
Appendix D. Main symbols
References
 
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5 . A simple scalar illustration of least-squares estimation

Let us assume that we need to estimate the temperature of a room.

We have a thermometer of known accuracy (the standard deviation of measurement error) and we observe , which is considered to have expectation (i.e. we assume that the observation is unbiased) and variance . In the absence of any other information the best estimate we can provide of the temperature is , with accuracy .

However we may have some additional information about the temperature of the room. We may have a reading from another, independent thermometer, perhaps with a different accuracy. We may notice that everyone in the room is wearing a jumper-another timely piece of information from which we can derive an estimate, although with a rather large associated error. We may have an accurate observation from an earlier date, which can be treated as an estimate for the current time, with an error suitably inflated to account for the separation in time. Any of these observations could be treated as a priori or background information, to be used with in estimating the room temperature. Let our background estimate be , of expectation (i.e. it is unbiased) and of accuracy . Intuitively and can be combined to provide a better estimate (or analysis) of than any of these taken alone. We are going to look for a linear weighted average of the form:

 

which can be rewritten as , i.e. we look for a correction to the background which is a linear function of the difference between the observation and the background.

The error variance of the estimate is:

 

where we have assumed that the observation and background errors are uncorrelated. We choose the optimal value of that minimizes the analysis error variance:

 

which is equivalent to minimizing (Fig. 5 )

 



Figure 5 . Schematic representation of the variational form of the least-squares analysis, in a scalar system where the observation is in the same space as the model : the cost-function terms and are both convex and tend to "pull" the analysis towards the background and the observation , respectively. The minimum of their sum is somewhere between and , and is the optimal least-squares analysis.
    In the limiting case of a very low quality measurement ( ), and the analysis remains equal to the background.
    On the other hand, if the observation has a very high quality ( ), and the analysis is equal to the observation.
    If both have the same accuracy, , and the analysis is simply the average of and , which reflects the fact that we trust as much the observation as the background, so we make a compromise.
    In all cases, , which means that the analysis is a weighted average of the background and the observation.
These situations are sketched in Fig. 6 .


Figure 6 . Schematic representation of the variations of the estimation error , and of the optimal weight that determines the analysis , for various relative amplitudes of the background and observation standard errors ( ).

It is interesting to look at the variance of analysis error for the optimal :

 

or

 

which shows that the analysis error variance is always smaller than both the background and observation error variances, and it is smallest if both are equal, in which case the analysis error variance is half the background error variance.


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