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The Interaction of Jet Streak Circulations during Heavy Snow Events along the East Coast of the United States
1987
Weather and forecasting
The interaction of transverse vertical circulations associated with two separate jet streak/trough systems is found to be a common feature of cyclogenetic events which produce heavy snow along the East Coast of the United States. The transverse circulations are identified for eight cases that span the period from 1960 to 1987 utilizing an isentropic analysis of the operational radiosonde data. The analyses depict the interaction of 1) a direct circulation located within the confluent entrance
doi:10.1175/1520-0434(1987)002<0289:tiojsc>2.0.co;2
fatcat:hopfqdvqtrb6bglcqh4jccm2au