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Bulletin American Meteorological Society 303 The development of Doppler weather radars (Gray Gray, G. R., R. J. Serafin, D. Atlas, R. E. Rinehart, and J. J. et al., 1975) that can detect tornado vortices presents an Boyajian, 1975: Real-time color Doppler radar display. exciting opportunity to develop very effective tornado Bull. Amer. Meteor. Soc., 56, 581-588. warning systems. As in the case of the visual sightings, Hering, W. S., H. A. Brown, and H. S. Muench, 1972: Meso- the Doppler radar can detect the phenomenon itself, scale forecast experiments. Bull. Amer. Meteor. Soc., 53, and it has the advantages that the incipient tornadoes 1180-1183. can be detected aloft well before touching ground (Don- Howe, O. M., 1974: Tornado path sizes. J. Appl. Meteor., 13, aldson, 1975), and detection can be made both day 343-347. and night. It is almost certain that the severe weather Mogil, H. M., 1974: Evaluation of severe weather and thun- forecaster working with Doppler information will also derstorm forecasts using manually digitized radar data and the SELS severe weather log. Preprints, Fifth Conference on have to make fast analyses and fast decisions; he will Weather Forecasting Analysis, Boston, Amer. Meteor. Soc., welcome computer guidance. Without speculating on the 270-275. form of this guidance, we can say that "radar plus com- Moore, P. L., A. D. Cummings, and D. L. Smith, 1974: The puter (plus forecaster?) equals fast diagnosis and National Weather Service manually digitized radar program warning." and its application to precipitation probability forecast- References ing. Preprints, Fifth Conference on Weather Forecasting and Analysis, Boston, Amer.
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