Experiments with the balance equation
DOI:
https://doi.org/10.54302/mausam.v26i3.2257Keywords:
Numerical experiments, stream function, geopotential field, balance-wind derived, geostrophic windAbstract
Numerical experiments were performed to solve the balance equation for obtaining the stream function from the geopotential field. The balance-wind derived from the balance is then compared with geostrophic wind. It is observed that the computed balance-wind appears to be a better approximation to the observed wind field than the geostrophic wind derived from the observed geopotential.
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