A diagnostic multi-level, non-linear balance model, which can be
used in either tropical or mid-latitude regions, is applied to a case
study in a mid-latitude region on 15, 16 and 17 November 1966. The
model accepts actual geopotential heights or geopotentil heights
derived from a non-divergent stream function which is computed from
the actual wind field as input data. A comparison is made between non-divergent stream functions
computed from the wind field and those computed from the actual
geopotential height field. A second comparison is made between the
actual geopotential height field and the geopotential height field
computed from the wind field. Qualitative and quantitative comparisons
are made between the stream functions and geopotential heights,
respectively, computed by the two different methods. By making the above mentioned comparisons, a determination is
made as to the accuracy of the model using wind data and finally the
accuracy of the model in the tropics , The results indicate that use of
the wind field as input data may not produce accurate results.Lieutenant, United States Navyhttp://archive.org/details/acomparisonofgeo109451180
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