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The first person to gain public recognition as a storm chaser was David Hoadley (born 1938), who began chasing North Dakota storms in 1956, systematically using data from area weather offices and airports.
Idealized depiction of where a dryline is located around an extratropical cyclone. A dry line (also called a dew point line, or Marfa front, after Marfa, Texas) [1] is a line across a continent that separates moist air and dry air.
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