Abstract
The adiabatic and diabatic vertical velocities at 800, 600 and 400 mb surfaces were computed using 4-level geostrophic baroclinic model over the Indian region. The smoothing of initial height field in time and space following Shuman's technique has been done at each of the four levels 900, 700, 500 and 300 mbs. The vertical velocities computed by using smoothed and unsmoothed height data have been compared.
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