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Assimilation algorithm: application to MSDOL

Assumptions:

o     The observation errors are spatially and temporally uncorrelated. This allows to handle each observation separately;

o     The horizontal and vertical forecast error covariances are independent and the vertical forecast error covariance is neglected;

o     Only the time evolution of the diagonal elements (the variances) of the forecast error covariance matrix are computed;

o     The covariances are computed by assuming that the horizontal correlation of the forecast error field may be represented by a simple function of the distance;

o     The operator H is a bilinear interpolation acting on the four points of the model surrounding the location of the observation.


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