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ESS124
Prof. Jin-Yi Yu
• Gulf Coast cyclones are more likely to track northward along the Mississippi Vally when the upper-level trough is farther west over the central US prior to their formation and the airflow across the eastern third of the US is southerly.
•The subtropical jetstream merges into the polar jetstream east of the trough axis.
•Cyclones forming in this environment is usually weaker in intensity than their costal counterparts.
Fig
Mississippi-Ohio River Valley Storm Track
•The cyclone first develops along the cold front.
•As the cyclone tracks northward, freezing rain and heavy snow occur north of the advancing warm front and in the northwest of the low-pressure center.
•Floods may occur in the southeast sectors of the low due to moist airs.