A dry line is a boundary between humid air from the Gulf of Mexico and dry air from the Rockies.
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Dry lines are one of the few surface fronts where the pips indicated do not necessarily reflect the direction of motion.
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In dry lining, the company sells eco-friendly gypsum fiber wallboard under the brands Fermacel and Aestuver for insulation and fire protection.
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Seasoned American meteorologists will know the ebb and flow of cold fronts, supercells, dry lines and other denizens of the meteorological menagerie.
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Approaching the dry line on the table are located low vacuum boxes that are drained by a barometric leg under gravity pressure.
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During spring and summer, humidity can rise and fall dramatically in the southern Plains whenever a dry line wavers across the region.
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A dry line is depicted on United States surface analyses as a brown line with scallops, or bumps, facing into the moist sector.
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Maximized pressure falls ahead of the dry line allowed several storms to acquire intense updrafts and develop into rotating supercells within the state.
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A maritime Polar ( mP ) cold front draped southwestward across eastern Texas with a dry line forming due south of the low.
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Further south in Oklahoma, a rapidly mixing dry line accompanied by a deepening surface low moved eastward into an area with deep moisture.
