A NOTE ON THE NON-UNIQUENESS OF THE UMKEHR METHOD B.
EMMANUEL COLL BOSTON MASS ORIENTAL SCIENCE LIBRARY
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The umkehr method B is used to determine the fine structure of the vertical distribution of atmospheric ozone. Essentially, the curve representing the vertical ozone distribution is continuous and smooth. In the method B, a block distribution diagram is used to replace this continuous curve. An optimum block distribution diagram is then obtained by the method of successive approximation. Based on the trend of variation of the optimum block diagram, the smooth curve connecting the areas may be considered approximately as the curve for the vertical ozone distribution.
- Atmospheric Physics