False, A warm front is predicted to come through your area tomorrow. You should prepare for thunderstorms, hail, and tornadoes
A warm front is a density discontinuity that is usually found on the edge of an isotherm gradient that faces the equator and is situated at the leading edge of a homogeneous warm air mass.
After frontal passage, clearing and warming normally happen quickly. Thunderstorms may be imbedded in the stratiform clouds ahead of the front if the warm air mass is unstable, and they may persist after the front has passed.
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