Observations of a sharp cold front and closely associated squall line in New England are analyzed. A striking feature is a line of convective clouds and heavy precipitation, which does not extend above 10,000 ft. The radar indication of the true plan-position and vertical extent of such disturbances is of special importance to air operations.
Research Article| 21 August 2018
Observations of a Cold Front, 1 October 1958
Edwin Kessler, III;
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Kessler, E., and R. Wexler, 1960: Observations of a Cold Front, 1 October 1958. Bull. Amer. Meteor. Soc., 41, 253–257, https://doi.org/10.1175/1520-0477-41.5.253.
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