In data assimilation, one prepares the grid data as the best possible estim
ate of the true initial state of a considered system by merging various mea
surements irregularly distributed in space and time, with a prior knowledge
of the state given by a numerical model. Because it may improve forecastin
g or modeling and increase physical understanding of considered systems, da
ta assimilation now plays a very important role in studies of atmospheric a
nd oceanic problems. Here, three examples are presented to illustrate the u
se of new types of observations and the ability of improving forecasting or
modeling.