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METEOROLOGICAL CONDITIONS ASSOCIATED WITH THE DEVELOPMENT OF INSTABILITY LINES

John G. BreilandUniversity of New Mexico

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Abstract

Results obtained from a diagnostic study of instability lines are presented. The results indicate that an instability line is associated with low-level horizontal convergence brought about primarily by the variation of the isentropic upgliding motion associated with a layer of strong, confluent winds in the lower levels of the troposphere.

Abstract

Results obtained from a diagnostic study of instability lines are presented. The results indicate that an instability line is associated with low-level horizontal convergence brought about primarily by the variation of the isentropic upgliding motion associated with a layer of strong, confluent winds in the lower levels of the troposphere.

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