that warm air can rise up and over the cold air like a cap. Meteorologists sometimes refer to this as a “wedge” of warm air—and it’s key to the formation of freezing rain and ice pellets.
that warm air can rise up and over the cold air like a cap. Meteorologists sometimes refer to this as a “wedge” of warm air—and it’s key to the formation of freezing rain and ice pellets.
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