Conclusions
• Typically observations of surface soil moisture
must have an accuracy of better than 5% v/v.
• If model covariance forecasts are imperfect and
observation errors are large there may be a
slight degradation of the model forecast.
• To achieve the best results, it is important that
the model, model forcing and observations be
unbiased, or the bias modeled as part of the
assimilation framework.