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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.
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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