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Aircraft observations taken in the course of three flights of the Tornado Research Airplane on 11 June 1956 were analyzed. These flights were made over the eastern slope of the Rocky Mountains where a squall line was predicted. The analysis revealed the structure of a dry frontal surface which played an important role upon the development of the squall line.
1 The research here reported has been sponsored by the U. S. Weather Bureau under Contract Cwb 8950.
Aircraft observations taken in the course of three flights of the Tornado Research Airplane on 11 June 1956 were analyzed. These flights were made over the eastern slope of the Rocky Mountains where a squall line was predicted. The analysis revealed the structure of a dry frontal surface which played an important role upon the development of the squall line.
1 The research here reported has been sponsored by the U. S. Weather Bureau under Contract Cwb 8950.
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