1969 Volume 47 Issue 2 Pages 115-124
The author's previous study on an objective analysis method (1958) is extended, by introducing terms of time variation and the dynamical equations which describe the time variation, for the purposes : 1) to filter and suppress unnecessary meteorological high frequency noises contained in the initial data and forecast fields and 2) to obtain the dynamically sound initial values for the areas or layers of lacking observation. The fundamental concept of the method is explained using the most simple examples of dynamical constraints; linear advection and linear diffusion.